Our survey of laboratory activities showed that work with compressed gases and flammable liquids was in acceptable compliance with security considerations and safe work procedures. However, the above half of non-compliance was related to the preparation in emergency response situations, not using personal protective equipment, poor inappropriate chemical disposal, treatment of waste products, and awareness and training. The lack of written emergency action plans, chemical hygiene lab procedures, and Safety Data Sheet (SDS) were identified to contribute to operational risks in chemical laboratory activities. The unsafe acts by the lab staff related to waste effluent disposal management mainly included risk factors of improper disposal containment and methods for experiment waste. We observed a lack of compliance in emergency response plans that are mainly associated with inadequate knowledge of staff and students about how to identify the location of fire extinguishers, how to request emergency assistance, and how to communicate potential leak, fire, and explosion scenarios. The unsafe conditions, such as aging electrical cords and plugs and contact with incorrectly grounded devices, were identified to increase operational risks of instruments in laboratories. Additionally, obstructed fire alarm pull stations or inappropriate layout of fire extinguishers in the lab environments increases the reaction time in the occurrence of accidents. Almost all individuals involved in handling chemicals in the laboratories reported they had not received the proper chemical safety training. Our onsite observations showed the unsafe storage of chemicals, which may lead to leakage and increase the possibility of exposure and accidents or high potential for injuries and damages. Students and laboratory workers were more likely not to choose the safe course of action concerning the use of personal protective equipment. For example, a common unsafe act was working in university labs without wearing face and eye or respiratory protection. The absence of proper Protective Personal Equipment (PPE) leads to unsafe exposure and subsequent injury. Furthermore, in chemical laboratories, the users frequently violated safe work procedures during transporting or setting up the experiment or apparatus. We identified many facilities and experiments in compliance with environment, health, and safety codes for handling flammable liquids and compressed gases in chemical laboratories. However, any deviation from the intended experimental steps in laboratory operations could result in severe consequences. The survey evaluated comprehensive health, safety, and environmental hazards of 54 chemicals used in chemical laboratories ( Figure 2 ). The proposed class-based risk assessment involves five levels of classes. The fourth- and fifth-level classes characterize the main risk factors.
Frequency of chemicals at estimated risk level classes in university laboratory activities.
A total of 44 risk factors were predicted and recognized as the “high” or “very high” level assessment classes. Potential health hazards recognized at the “very high” level were more frequent when compared to safety and environmental hazards, respectively, accounting for 9.2, 3.7, and 1.8% of the total number of hazards at the “very high” level class. Moreover, the chemicals with the level of “high” risk contributed to a greater number of environmental hazards (35.2%) followed by safety hazards (20.4%) and health hazards (11.1%). The identified health, safety, and environmental hazards of chemicals at the intermediate level were, respectively, 20.4, 13, and 18.5% of the total number of third-level categories, implying that prevention and control actions are required to manage the risks. Additionally, the mean value of 29.7% of the assessed chemicals had very low and low health risk levels. These mean values for safety and environmental hazards were 31.5 and 22.3%, respectively.
Overall, using chemicals in laboratory operations produced a wide range of risk levels. Cyclohexane, Nitric acid, Sulfuric acid, Formaldehyde, and Sodium Hydroxide were classified as “very high” risk levels with a score estimated at 25, accounting for 9.3% of potential hazards to health. Many chemicals (35.2%) were classified at the “high” risk levels involved in environmental hazards. In contrast, few chemicals (1.8%) presented a “very high” risk level to the environment. Table 3 demonstrates the potential health, safety, and environmental hazards of the studied chemicals and the relevant calculated risk scores.
Health, safety, and environmental risk assessment matrix of common chemicals used in university laboratories.
Acetone | 4 | 1 | 4 | 4 | 5 | 20 | 4 | 3 | 12 |
Acetic acid | 4 | 4 | 16 | 3 | 4 | 12 | 4 | 3 | 12 |
Ethanol | 5 | 3 | 15 | 5 | 5 | 25 | 5 | 3 | 15 |
Ammoniac | 4 | 5 | 20 | 3 | 5 | 15 | 4 | 4 | 16 |
Benzene | 3 | 3 | 9 | 4 | 4 | 16 | 3 | 5 | 15 |
Butanol | 4 | 4 | 8 | 4 | 5 | 20 | 2 | 2 | 4 |
Chloroform | 4 | 5 | 20 | 4 | 5 | 20 | 2 | 3 | 6 |
Cyclo hexanol | 3 | 2 | 6 | 3 | 5 | 15 | 3 | 2 | 6 |
Hydrochloric acid | 5 | 5 | 25 | 5 | 4 | 20 | 5 | 5 | 25 |
Hydrogen peroxide | 4 | 4 | 16 | 4 | 3 | 12 | 4 | 4 | 16 |
Methanol | 3 | 5 | 15 | 5 | 4 | 20 | 3 | 2 | 6 |
Nitric acid | 5 | 4 | 20 | 4 | 4 | 16 | 5 | 5 | 25 |
Sulfuric acid | 5 | 4 | 20 | 5 | 5 | 25 | 5 | 5 | 25 |
Di chloromethane | 4 | 1 | 4 | 4 | 2 | 8 | 3 | 3 | 9 |
Di ethyl ether | 3 | 3 | 9 | 4 | 5 | 20 | 3 | 2 | 6 |
Ethylene glycol | 2 | 2 | 4 | 2 | 2 | 4 | 2 | 3 | 6 |
Formaldehyde | 4 | 5 | 20 | 3 | 4 | 12 | 5 | 5 | 25 |
Isopropanol | 3 | 3 | 9 | 4 | 4 | 16 | 3 | 2 | 6 |
Orto toluidine | 1 | 5 | 5 | 2 | 4 | 8 | 1 | 4 | 4 |
Toluene | 3 | 3 | 9 | 4 | 4 | 20 | 3 | 3 | 9 |
Carbon disulfide | 4 | 3 | 12 | 4 | 5 | 20 | 3 | 4 | 12 |
Paraffin | 4 | 1 | 4 | 1 | 2 | 2 | 2 | 2 | 4 |
Aluminum sulfate | 4 | 4 | 16 | 1 | 3 | 3 | 3 | 3 | 9 |
Arsenic oxide | 2 | 5 | 10 | 3 | 3 | 9 | 2 | 5 | 10 |
Barium chloride | 2 | 5 | 10 | 1 | 2 | 2 | 2 | 3 | 6 |
Cadmium chloride | 3 | 5 | 15 | 1 | 2 | 2 | 3 | 5 | 15 |
Iodine | 4 | 5 | 20 | 2 | 2 | 4 | 5 | 4 | 20 |
Ferric sulfate | 3 | 4 | 12 | 1 | 3 | 3 | 3 | 3 | 9 |
Ferric chloride | 3 | 3 | 9 | 2 | 1 | 2 | 3 | 4 | 12 |
Ammonium carbonate | 2 | 5 | 10 | 2 | 4 | 8 | 2 | 3 | 6 |
Ammonium chloride | 2 | 2 | 4 | 2 | 1 | 2 | 2 | 3 | 6 |
Asbestos | 4 | 4 | 8 | 2 | 4 | 8 | 1 | 5 | 5 |
Brome | 2 | 5 | 10 | 3 | 3 | 9 | 2 | 4 | 8 |
Calcium carbonate | 3 | 1 | 3 | 1 | 1 | 1 | 3 | 3 | 9 |
Calcium hydroxide | 3 | 4 | 12 | 1 | 3 | 3 | 3 | 4 | 12 |
Magnesium oxide | 2 | 5 | 10 | 1 | 2 | 2 | 2 | 3 | 6 |
Phenol | 4 | 5 | 20 | 2 | 3 | 6 | 2 | 5 | 10 |
Manganese sulfate | 4 | 5 | 20 | 1 | 2 | 2 | 2 | 4 | 8 |
Potassium hydroxide | 5 | 4 | 20 | 3 | 3 | 9 | 5 | 4 | 20 |
Silver nitrate | 3 | 5 | 15 | 2 | 3 | 6 | 3 | 4 | 12 |
Sodium azide | 1 | 5 | 5 | 3 | 2 | 6 | 1 | 4 | 4 |
Sodium fluoride | 3 | 5 | 15 | 2 | 2 | 4 | 3 | 4 | 12 |
Sodium hydroxide | 5 | 4 | 20 | 3 | 3 | 9 | 5 | 5 | 25 |
Mercury | 4 | 5 | 20 | 2 | 3 | 6 | 2 | 4 | 8 |
Potassium cyanide | 4 | 5 | 20 | 3 | 4 | 12 | 2 | 4 | 8 |
Sodium cyanide | 1 | 5 | 5 | 2 | 3 | 6 | 1 | 4 | 4 |
Potassium chromate | 4 | 5 | 20 | 2 | 3 | 6 | 5 | 4 | 20 |
Tin chloride | 4 | 5 | 20 | 2 | 3 | 6 | 4 | 4 | 16 |
Citric acid | 2 | 2 | 4 | 1 | 2 | 2 | 2 | 2 | 4 |
Cobalt chloride | 4 | 5 | 20 | 2 | 3 | 6 | 2 | 4 | 8 |
Lead acetate | 1 | 5 | 5 | 2 | 2 | 4 | 1 | 3 | 3 |
Lead nitrate | 1 | 5 | 5 | 2 | 4 | 8 | 1 | 4 | 4 |
Mercury chloride | 4 | 5 | 20 | 3 | 5 | 15 | 1 | 5 | 5 |
Nitrate nickle | 1 | 5 | 5 | 2 | 4 | 8 | 1 | 3 | 3 |
Our risk assessment showed that 25.9% of the laboratory chemicals might be associated with heavy potential exposure as scored at 5 or 4. Moreover, more than half of the laboratory chemicals (25.9%) contributed to the high level of severity outcomes. The results demonstrated that Ethanol and Sulfuric acid presented a “very high” risk level (scored at 25) in safety risk assessment. Furthermore, 27.8 and 44.4% of chemicals were rated high scores of probability and severity, respectively, in the safety risk assessment. Hydrochloric acid was the only chemical that was ranked at the “very high” level in the environmental risk assessment, with a score estimated at 25.
This study assessed health, safety, and environmental risks in academic laboratories that use chemicals for educational and research activities. The variability of chemical use in academic laboratories might lead to various health, safety, and environmental risk factors. Our findings agree with prior research that suggested that educational and research laboratories of academic institutions need to assess their vulnerabilities and plan their own risk mitigation accordingly ( 20 ).
Our risk assessment indicated that the percentage of health hazards at the “very high” risk level was higher when compared to the safety and environmental hazards. Overall, the mean values of 13.6, 12.4, and 18.5% of the assessed chemicals were classified in “moderate” to “very high” categories of health, safety, and environmental hazards, respectively. Therefore, health and safety rules must be considered strictly as a priority by the people who work with chemicals in laboratories for reducing the risk of chemical-related diseases and accidents ( 21 ). In this study, the laboratory health and safety checklist showed that most non-compliance was linked to the chemical storage and training/awareness sections. The main faults in chemical storage were related to the labeling of cabinets to indicate chemical class and the labeling of chemical containers, particularly when chemicals are transferred from their original containers. Additionally, quantities of chemicals in storage were inconsistent with short-term needs of the assessed laboratories. All of these non-compliances in chemical storage may result in extensive fire or explosion in the laboratories of academic settings. Omidvari et al. found similar results in their study at Azad University in Iran, which reported fire risk and accidents in educational buildings, particularly in laboratories ( 22 ).
Due to the importance of training and awareness in reducing exposures, accidents, and injuries, all laboratory workers, such as faculty, staff, and students, should receive laboratory standard training. The training programs should involve chemical safety programs, chemical emergency action plans, and laboratory security plans. After holding the training courses, it should be ensured that the laboratory workers know who and when to use personal protective equipment, how to use emergency equipment, such as eyewashes and safety showers, where SDSs are kept, spill control procedures, emergency procedures, and chemical waste procedures. The previous studies recommended the periodic training courses for laboratory staff and approved the laboratory safety and security curriculum in most faculties in order to increase awareness, safety, and security culture among laboratory workers and allow them to distinguish what to do before, during, and after emergencies ( 9 , 23 – 25 ).
Moreover, the general work environment, emergency planning, and required information for chemical laboratories were the other parts of the checklist that involved the highest numbers of non-compliance in this study. Not only allocating one room of the chemistry laboratory to a chemical warehouse has been increased the safety risk but also the layout of chemicals was not in accordance with safety principles and standards for practice. For instance, the chemical storage was not at “least 18 below the sprinkler head or at least 24” below the ceiling. In at least 2 laboratories, not considering the 5S principles for work environment and storage of materials, such as paper goods, plastic containers, boxes, and empty containers, that would fuel to the burning fire was major non-compliance violation. Additionally, the alternative exits, chemicals material safety data sheet (MSDS), safety instructions, Self-Contained Breathing Apparatus (SCBA), and required special security systems or controls to limit access were not available in the assessed laboratories. The lack of an emergency action plan was the other major fault in this study. The findings of this study and similar research studies provide useful information to plan and develop an emergency action plan for the prevention and mitigation of the emergencies and their harmful consequences in the laboratories of academic institutions ( 26 – 28 ). The prevention and mitigation measures should be prioritized for implementation in accordance with available funds and other resources. Prior studies reported low-cost interventions that might involve reducing major risks and their consequences. Planning a safe layout for gas cylinders or fire extinguishers, providing the SDS for all chemicals used in laboratories, using chemical labeling of cabinets and containers, and non-structural mitigation measures are recommended ( 29 , 30 ).
In the domain of environmental risk assessment, 44.5% of chemicals were classified in “very low” and “low' risk levels, but 55.5% of them were ranked “intermediate” to “very high” risk degrees. The most important chemical environment-related hazard was waste disposal. The lack of an individual sewage system for laboratories and releasing chemicals into the urban sewage system can contaminate the underground water with hazardous chemicals. Previous studies assessed a high level of environmental risk in underground water reservoirs related to hazardous chemical effluents from academic laboratories ( 31 , 32 ).
This chemical health, safety, and environmental risk assessment was developed and conducted according to the standards and guidelines set by the international occupational health and safety organizations. The applied approach revealed the significant risks associated with chemicals used at the university laboratories. The instrument developed for this study will be put into good use in helping health and safety engineers to identify and classify potential risks of laboratory operations to health, safety, and environment. Prevention and mitigation measures should be based on detailed risk assessment methods to minimize identified hazards and provide a safe environment to reduce and/or eliminate the occurrence of diseases and injury in laboratories.
Universities should provide training courses in the curriculum on health and safety in laboratories, particularly for new students at the first of each semester, and periodic similar training courses for faculty and staff plays a key role in increasing awareness and risk perception for considering significant risks at the laboratories. Furthermore, inspecting and assessing the laboratories and research facilities by standard laboratory checklists routinely and removing the non-compliance operations at the earliest time are essential in providing a safe work environment.
Ethics statement.
This study was approved by the Ethics Committee Review Board at Semnan university of Medical Sciences (IR.SEMUMS.REC.1398.131). All the participants signed a consent form and were informed on the purpose of the study prior to interview as per local protocol on research ethics.
AD: material preparation, conceptualization, methodology, investigation, writing—reviewing, and editing. MJ: material preparation, conceptualization, and data collection. FF: analysis, interpretation, first draft of the manuscript, conceptualization, and investigation. All authors contributed to the study conception, design, investigation, reviewed and commented on previous versions of the manuscript, and read and approved the final manuscript.
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.
The authors would like to thank all the staff laboratories that participated and collaborated in this study and Semnan University of Medical Sciences and Health Services for their support to conduct this research.
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Increasing wildfire risk is a major menace to the subtropical biodiversity. However, regional plan may not oblige the local management in wildfire prevention in a locality where people are majorly depending on forest resource and the area undergoes significant human encroachment. Addressing that, the current study focuses one such area, Hoshangabad Forest Division (HFD), located in Central India, where wildfires have damaged the local biodiversity and surrounding socio-economic activities in previous years. While several studies found alarming increase in wildfires across different regions in India, this study found a non-significant increasing trend (slope = ~ 1 incidence/year) of MODIS active fire points over HFD area. Positive and significant spatial autocorrelation among the fire locations was found (Moron's I = 0.11), which indicates that fire often ignite over few specific places and spread to neighboring areas. Using Getis-Ord Gi statistics, four significant hotspots were distinguished, where 47% of total fire occurrences had occurred and the remaining were observed scattered across HFD. To assess wildfire risk within this locality, Analytical Hierarchical Process was used, where eight physical and six socio-economic factors were integrated in GIS environment. The model achieved a ROC-AUC score of 0.76 while validated with wildfire records from the MODIS. 32 and 28% of HFD area were found under high and very high-risk, respectively, where 78% of wildfire incidents had occurred during 2001–2022. Additionally, specific areas within HFD (western, central west, and south-western areas) are identified as facing higher risks of wildfires. This study shows that wildfire risk assessment at local-scale may differ what observed a regional scale and provide a promenade for area-specific wildfire prevention plan. It also suggests enhanced monitoring near forest edges, immediate action to protect teak trees, and prescribed fire management to reduce dry fuel in forests and roadsides. Thus, the study provides valuable insights into wildfire management and contributes to more specialized research and methodological advancement in this field.
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Abdo, H. G., Almohamad, H., Al Dughairi, A. A., & Al-Mutiry, M. (2022). GIS-based frequency ratio and analytic hierarchy process for forest fire susceptibility mapping in the western region of Syria. Sustainability, 14 (8), 4668. https://doi.org/10.3390/su14084668
Article Google Scholar
Abedi Gheshlaghi, H. (2019). Using GIS to develop a model for forest fire risk mapping. Journal of the Indian Society of Remote Sensing, 47 (7), 1173–1185. https://doi.org/10.1007/s12524-019-00981-z
Adab, H., Kanniah, K. D., & Solaimani, K. (2013). Modeling forest fire risk in the northeast of Iran using remote sensing and GIS techniques. Natural Hazards, 65 (3), 1723–1743. https://doi.org/10.1007/s11069-012-0450-8
Afreen, S., Sharma, N., Chaturvedi, R. K., Gopalakrishnan, R., & Ravindranath, N. H. (2011). Forest policies and programs affecting vulnerability and adaptation to climate change. Mitigation and Adaptation Strategies for Global Change, 16 (2), 177–197. https://doi.org/10.1007/s11027-010-9259-5
Aftergood, O. S. R., & Flannigan, M. D. (2022). Identifying and analyzing spatial and temporal patterns of lightning-ignited wildfires in Western Canada from 1981 to 2018. Canadian Journal of Forest Research, 52 (11), 1399–1411. https://doi.org/10.1139/cjfr-2021-0353
Ajin, R., Loghin, A.-M., Vinod, P., & Jacob, M. (2016). Forest Fire risk zone mapping using RS and GIS techniques: A study in Achankovil Forest Division, Kerala, India. Journal of Earth, Environment and Health Sciences, 2 (3), 109. https://doi.org/10.4103/2423-7752.199288
Aragão, L. E. O. C., Anderson, L. O., Fonseca, M. G., Rosan, T. M., Vedovato, L. B., Wagner, F. H., Silva, C. V. J., Silva Junior, C. H. L., Arai, E., Aguiar, A. P., Barlow, J., Berenguer, E., Deeter, M. N., Domingues, L. G., Gatti, L., Gloor, M., Malhi, Y., Marengo, J. A., Miller, J. B., Saatchi, S. (2018). 21st Century drought-related fires counteract the decline of Amazon deforestation carbon emissions. Nature Communications , 9 (1), 536. https://doi.org/10.1038/s41467-017-02771-y
Babu, K. S., Roy, A., & Aggarwal, R. (2018). Mapping of forest fire burned severity using the sentinel datasets. The International Archives of Photogrammetry, Remote Sensing and Spatial Information Sciences, 42 , 469–474.
Babu, K. V., Roy, S. A., & Prasad, P. R. (2016). Forest fire risk modeling in Uttarakhand Himalaya using TERRA satellite datasets. European Journal of Remote Sensing, 49 (1), 381–395. https://doi.org/10.5721/EuJRS20164921
Behera, S., Prusty, B. K., Behera, M. D., & Kale, M. P. (2023). Characterizing fuel flammability in a tropical dry community forest in Eastern India using laboratory and remote sensing based approaches. Tropical Ecology . https://doi.org/10.1007/s42965-023-00309-6
Belikova, M. Y., Baranovskiy, N. V., Karanin, A. V., Bazarov, A. V., Sychev, R. S., & Glebova, A. V. (2022). Analysis of Spatial Distribution Processes for Forest Fires Near the Railway Infrastructure Using Clustering: Case Study. International Journal on Engineering Applications (IREA) , 10 (6), Article 6. https://doi.org/10.15866/irea.v10i6.22224
Bhuyan, M. J., & Deka, N. (2022). Delineation of groundwater potential zones at micro-spatial units of Nagaon district in Assam, India, using GIS-based MCDA and AHP techniques. Environmental Science and Pollution Research . https://doi.org/10.1007/s11356-022-24505-4
Bhuyan, M. J., Deka, N., & Saikia, A. (2024). Micro-spatial flood risk assessment in Nagaon district, Assam (India) using GIS-based multi-criteria decision analysis (MCDA) and analytical hierarchy process (AHP). Risk Analysis, 44 (4), 817–832. https://doi.org/10.1111/risa.14191
Cetin, M., Isik Pekkan, Ö., Ozenen Kavlak, M., Atmaca, I., Nasery, S., Derakhshandeh, M., & Cabuk, S. N. (2023). GIS-based forest fire risk determination for Milas district. Turkey. Natural Hazards, 119 (3), 2299–2320. https://doi.org/10.1007/s11069-022-05601-7
Cetin, M., Kaya, A. Y., Elmastas, N., Adiguzel, F., Siyavus, A. E., & Kocan, N. (2024). Assessment of emergency gathering points and temporary shelter areas for disaster resilience in Elazıg. Turkey. Natural Hazards, 120 (2), 1925–1949. https://doi.org/10.1007/s11069-023-06271-9
Chandramouli, C., & General, R. (2011). Census of india 2011. Provisional Population Totals. New Delhi: Government of India , pp. 409–413.
Chas-Amil, M. L., Touza, J., & García-Martínez, E. (2013). Forest fires in the wildland–urban interface: A spatial analysis of forest fragmentation and human impacts. Applied Geography, 43 , 127–137. https://doi.org/10.1016/j.apgeog.2013.06.010
Costa-Saura, J. M., Bacciu, V., Ribotta, C., Spano, D., Massaiu, A., & Sirca, C. (2022). Predicting and Mapping Potential Fire Severity for Risk Analysis at Regional Level Using Google Earth Engine. Remote Sensing , 14 (19), Article 19. https://doi.org/10.3390/rs14194812
Davis, E. J., Moseley, C., Nielsen-Pincus, M., & Jakes, P. J. (2014). The community economic impacts of large wildfires: A case study from Trinity County. California. Society and Natural Resources, 27 (9), 983–993. https://doi.org/10.1080/08941920.2014.905812
Dennison, P. E., Brewer, S. C., Arnold, J. D., & Moritz, M. A. (2014). Large wildfire trends in the western United States, 1984–2011. Geophysical Research Letters, 41 (8), 2928–2933. https://doi.org/10.1002/2014GL059576
Doerr, S. H., & Santín, C. (2016). Global trends in wildfire and its impacts: Perceptions versus realities in a changing world. Philosophical Transactions of the Royal Society B: Biological Sciences, 371 (1696), 20150345. https://doi.org/10.1098/rstb.2015.0345
Donegan, H. A., Dodd, F. J., & McMaster, T. B. M. (1992). A new approach to AHP decision-making. The Statistician, 41 (3), 295. https://doi.org/10.2307/2348551
Erden, T., & Karaman, H. (2012). Analysis of earthquake parameters to generate hazard maps by integrating AHP and GIS for Küçükçekmece region. Natural Hazards and Earth System Sciences, 12 (2), 475–483. https://doi.org/10.5194/nhess-12-475-2012
Ertugrul, M., Ozel, H. B., Varol, T., Cetin, M., & Sevik, H. (2019). Investigation of the relationship between burned areas and climate factors in large forest fires in the Çanakkale region. Environmental Monitoring and Assessment, 191 (12), 737. https://doi.org/10.1007/s10661-019-7946-6
Ertugrul, M., Varol, T., Ozel, H. B., Cetin, M., & Sevik, H. (2021). Influence of climatic factor of changes in forest fire danger and fire season length in Turkey. Environmental Monitoring and Assessment, 193 (1), 28. https://doi.org/10.1007/s10661-020-08800-6
Article CAS Google Scholar
Fernandes, P. M., & Botelho, H. S. (2003). A review of prescribed burning effectiveness in fire hazard reduction. International Journal of Wildland Fire, 12 (2), 117–128. https://doi.org/10.1071/wf02042
Flannigan, M. D., Wotton, B. M., Marshall, G. A., De Groot, W. J., Johnston, J., Jurko, N., & Cantin, A. S. (2016). Fuel moisture sensitivity to temperature and precipitation: Climate change implications. Climatic Change, 134 (1–2), 59–71. https://doi.org/10.1007/s10584-015-1521-0
Gabban, A., San-Miguel-Ayanz, J., & Viegas, D. X. (2008). A comparative analysis of the use of NOAA-AVHRR NDVI and FWI data for forest fire risk assessment. International Journal of Remote Sensing, 29 (19), 5677–5687. https://doi.org/10.1080/01431160801958397
Getis, A., & Ord, J. K. (1992). The analysis of spatial association by use of distance statistics. Geographical Analysis, 24 (3), 189–206. https://doi.org/10.1111/j.1538-4632.1992.tb00261.x
Ghosh, A., & Kar, S. K. (2018). Application of analytical hierarchy process (AHP) for flood risk assessment: A case study in Malda district of West Bengal. India. Natural Hazards, 94 (1), 349–368. https://doi.org/10.1007/s11069-018-3392-y
Gupta, A., Bhatt, C. M., Roy, A., & Chauhan, P. (2020a). COVID-19 lockdown a window of opportunity to understand the role of human activity on forest fire incidences in the Western Himalaya. India. Current Science, 119 (2), 390–398.
Gupta, A., Pradhan, B., & Maulud, K. N. A. (2020b). Estimating the impact of daily weather on the temporal pattern of COVID-19 outbreak in India. Earth Systems and Environment, 4 (3), 523–534. https://doi.org/10.1007/s41748-020-00179-1
Gupta, A., Roy, A., & Chauhan, P. (2023). Space-based observation of early summer wildfire event and its environmental proxies during 2021 in Eastern Peninsular India. Arabian Journal of Geosciences, 16 (7), 433. https://doi.org/10.1007/s12517-023-11544-5
Hussin, Y. A., Matakala, M., & Zagdaa, N. (2008). The application of remote sensing and GIS in modelling forest fire hazard in Mongolia. In ISPRS 2008 : Proceedings of the XXI congress : Silk road for information from imagery : the International Society for Photogrammetry and Remote Sensing, 3–11 July, Beijing, China. Comm. VIII, WG VIII/2. Beijing : ISPRS, 2008. pp. 289–294 (pp. 289–294). International Society for Photogrammetry and Remote Sensing (ISPRS). http://www.isprs.org/proceedings/XXXVII/congress/8_pdf/2_WG-VIII-2/22.pdf
Ionita, M., Nagavciuc, V., Scholz, P., & Dima, M. (2022). Long-term drought intensification over Europe driven by the weakening trend of the Atlantic Meridional Overturning Circulation. Journal of Hydrology: Regional Studies, 42 , 101176. https://doi.org/10.1016/j.ejrh.2022.101176
ISFR. (2021). Forest Survey of India, Ministry of Environment, Forest, and Climate Change (MoEFCC), Government of India. https://fsi.nic.in/forest-report-2021-details
Jafari Goldarag, Y., Mohammadzadeh, A., & Ardakani, A. S. (2016). Fire risk assessment using neural network and logistic regression. Journal of the Indian Society of Remote Sensing, 44 (6), 885–894. https://doi.org/10.1007/s12524-016-0557-6
Jain, M., Saxena, P., Sharma, S., & Sonwani, S. (2021). Investigation of forest fire activity changes over the central India domain using satellite observations during 2001–2020. GeoHealth , 5 (12), e2021GH000528.
Jain, P., Wang, X., & Flannigan, M. D. (2017). Trend analysis of fire season length and extreme fire weather in North America between 1979 and 2015. International Journal of Wildland Fire, 26 (12), 1009. https://doi.org/10.1071/WF17008
Jaiswal, R. K., Mukherjee, S., Raju, K. D., & Saxena, R. (2002). Forest fire risk zone mapping from satellite imagery and GIS. International Journal of Applied Earth Observation and Geoinformation, 4 (1), 1–10. https://doi.org/10.1016/S0303-2434(02)00006-5
Jiménez-Ruano, A., Rodrigues Mimbrero, M., Jolly, W. M., & De La Riva Fernández, J. (2019). The role of short-term weather conditions in temporal dynamics of fire regime features in mainland Spain. Journal of Environmental Management, 241 , 575–586. https://doi.org/10.1016/j.jenvman.2018.09.107
Kale, M. P., Ramachandran, R. M., Pardeshi, S. N., Chavan, M., Joshi, P. K., Pai, D. S., Bhavani, P., Ashok, K., & Roy, P. S. (2017). Are Climate Extremities changing forest fire regimes in India? An analysis using MODIS fire locations during 2003–2013 and gridded climate data of India Meteorological Department. Proceedings of the National Academy of Sciences, India Section a: Physical Sciences, 87 (4), 827–843. https://doi.org/10.1007/s40010-017-0452-8
Kant Sharma, L., Kanga, S., Singh Nathawat, M., Sinha, S., & Chandra Pandey, P. (2012). Fuzzy AHP for forest fire risk modeling. Disaster Prevention and Management: An International Journal, 21 (2), 160–171. https://doi.org/10.1108/09653561211219964
Kantarcioglu, O., Kocaman, S., & Schindler, K. (2023). Artificial neural networks for assessing forest fire susceptibility in Türkiye. Ecological Informatics, 75 , 102034. https://doi.org/10.1016/j.ecoinf.2023.102034
Kayet, N., Chakrabarty, A., Pathak, K., Sahoo, S., Dutta, T., & Hatai, B. K. (2020). Comparative analysis of multi-criteria probabilistic FR and AHP models for forest fire risk (FFR) mapping in Melghat Tiger Reserve (MTR) forest. Journal of Forestry Research, 31 (2), 565–579. https://doi.org/10.1007/s11676-018-0826-z
Kendall, M. (1975). Rank correlation methods . Charles Griffin & Co.
Google Scholar
Khan, H. U. (2013). Hoshangabad Forest Division’s Action Plan 2013–14 to 2022–23. Madhya Pradesh Forest Department , (380).
Kodandapani, N., Cochrane, M. A., & Sukumar, R. (2008). A comparative analysis of spatial, temporal, and ecological characteristics of forest fires in seasonally dry tropical ecosystems in the Western Ghats. India. Forest Ecology and Management, 256 (4), 607–617. https://doi.org/10.1016/j.foreco.2008.05.006
Kumar, A., Kumar, G., Saikia, P., Khare, P. K., & Khan, M. L. (2022). Spatial pattern of tree diversity and impacts of ecological disturbances on forest structure in tropical deciduous forests of Central India. Biotropica, 54 (6), 1363–1375. https://doi.org/10.1111/btp.13068
Kumar, M., Nisha Phukon, S., & Singh, H. (2021). The role of communities in sustainable land and forest management. In P. Kumar Shit, H. R. Pourghasemi, P. P. Adhikary, G. S. Bhunia, & V. P. Sati (Eds.), Forest Resources Resilience and Conflicts (pp. 305–318). Elsevier. https://doi.org/10.1016/B978-0-12-822931-6.00024-1
Kumar, S., & Kumar, A. (2022). Hotspot and trend analysis of forest fires and its relation to climatic factors in the western Himalayas. Natural Hazards, 114 (3), 3529–3544. https://doi.org/10.1007/s11069-022-05530-5
Kumar, S., Meenakshi, D. B., Vandana, G., & Kumar, A. (2015). Identifying triggers for forest fire and assessing fire susceptibility of forests in Indian western Himalaya using geospatial techniques. Natural Hazards, 78 (1), 203–217. https://doi.org/10.1007/s11069-015-1710-1
Kumari, B., & Pandey, A. C. (2020). Geo-informatics based multi-criteria decision analysis (MCDA) through analytic hierarchy process (AHP) for forest fire risk mapping in Palamau Tiger Reserve, Jharkhand state. India. Journal of Earth System Science, 129 (1), 204. https://doi.org/10.1007/s12040-020-01461-6
Lamat, R., Kumar, M., Kundu, A., & Lal, D. (2021). Forest fire risk mapping using analytical hierarchy process (AHP) and earth observation datasets: A case study in the mountainous terrain of Northeast India. SN Applied Sciences, 3 (4), 425. https://doi.org/10.1007/s42452-021-04391-0
Lasslop, G., & Kloster, S. (2017). Human impact on wildfires varies between regions and with vegetation productivity. Environmental Research Letters, 12 (11), 115011. https://doi.org/10.1088/1748-9326/aa8c82
Liu, Z., Yang, J., Chang, Y., Weisberg, P. J., & He, H. S. (2012). Spatial patterns and drivers of fire occurrence and its future trend under climate change in a boreal forest of Northeast China. Global Change Biology, 18 (6), 2041–2056. https://doi.org/10.1111/j.1365-2486.2012.02649.x
Madhya Pradesh Forest Department. (2017). Jurisdictional Sub-National Redd+ Program for Hoshangabad District of Madhya Pradesh State, India (Version 1.3). U.S. Agency for International Development . https://pdf.usaid.gov/pdf_docs/PA00N73S.pdf
Maffei, C., Lindenbergh, R., & Menenti, M. (2021). Combining multi-spectral and thermal remote sensing to predict forest fire characteristics. ISPRS Journal of Photogrammetry and Remote Sensing, 181 , 400–412. https://doi.org/10.1016/j.isprsjprs.2021.09.016
Mallick, J., Talukdar, S., Alsubih, M., Salam, R., Ahmed, M., Kahla, N. B., & Shamimuzzaman, Md. (2021). Analysing the trend of rainfall in Asir region of Saudi Arabia using the family of Mann-Kendall tests, innovative trend analysis, and detrended fluctuation analysis. Theoretical and Applied Climatology, 143 (1–2), 823–841. https://doi.org/10.1007/s00704-020-03448-1
Mamgain, S., Roy, A., Karnatak, H. C., & Chauhan, P. (2023). Satellite-based long-term spatiotemporal trends of wildfire in the Himalayan vegetation. Natural Hazards, 116 (3), 3779–3796.
Mamuji, A. A., & Rozdilsky, J. L. (2019). Wildfire as an increasingly common natural disaster facing Canada: Understanding the 2016 Fort McMurray wildfire. Natural Hazards, 98 (1), 163–180. https://doi.org/10.1007/s11069-018-3488-4
Mann, H. B. (1945). Nonparametric tests against trend. Econometrica, 13 (3), 245. https://doi.org/10.2307/1907187
Memisoglu Baykal, T. (2023). GIS-based spatiotemporal analysis of forest fires in Turkey from 2010 to 2020. Transactions in GIS, 27 (5), 1289–1317. https://doi.org/10.1111/tgis.13066
Mohammad, L., Mondal, I., Bandyopadhyay, J., Pham, Q. B., Nguyen, X. C., Dinh, C. D., & Al-Quraishi, A. M. F. (2022). Assessment of spatio-temporal trends of satellite-based aerosol optical depth using Mann-Kendall test and Sen’s slope estimator model. Geomatics, Natural Hazards and Risk, 13 (1), 1270–1298. https://doi.org/10.1080/19475705.2022.2070552
Mohammadi, F., Bavaghar, M. P., & Shabanian, N. (2014). Forest fire risk zone modeling using logistic regression and GIS: An Iranian case study. Small-Scale Forestry, 13 (1), 117–125. https://doi.org/10.1007/s11842-013-9244-4
Mohanty, A., & Mithal, V. (2022). Managing Forest Fires in a Changing Climate (p. 24). Council on Energy, Environment and Water New Delhi.
Mohd, A., Pritee, S., & Mohanasundari, T. (2024). Analysing the Escalation of Forest Fire in India: Exploring Causal Factors and Mitigation Strategies. Journal of Tropical Forest Science , 36 (2), 215–223. https://doi.org/10.26525/jtfs2024.36.2.215
Moran, P. A. P. (1950). Notes on continuous stochastic phenomena. Biometrika, 37 (1/2), 17. https://doi.org/10.2307/2332142
Narayanaraj, G., & Wimberly, M. C. (2012). Influences of forest roads on the spatial patterns of human- and lightning-caused wildfire ignitions. Applied Geography, 32 (2), 878–888. https://doi.org/10.1016/j.apgeog.2011.09.004
Nasiri, V., Sadeghi, S. M. M., Bagherabadi, R., Moradi, F., Deljouei, A., & Borz, S. A. (2022). Modeling wildfire risk in western Iran based on the integration of AHP and GIS. Environmental Monitoring and Assessment, 194 (9), 644. https://doi.org/10.1007/s10661-022-10318-y
Nezval, V., Andrášik, R., & Bíl, M. (2022). Vegetation fires along the Czech rail network. Fire Ecology, 18 (1), 15. https://doi.org/10.1186/s42408-022-00141-8
Nikhil, S., Danumah, J. H., Saha, S., Prasad, M. K., Rajaneesh, A., Mammen, P. C., Ajin, R. S., & Kuriakose, S. L. (2021). Application of GIS and AHP method in forest fire risk zone mapping: A study of the Parambikulam Tiger Reserve, Kerala, India. Journal of Geovisualization and Spatial Analysis, 5 (1), 14. https://doi.org/10.1007/s41651-021-00082-x
Nuthammachot, N., & Stratoulias, D. (2021). Multi-criteria decision analysis for forest fire risk assessment by coupling AHP and GIS: Method and case study. Environment, Development and Sustainability, 23 (12), 17443–17458. https://doi.org/10.1007/s10668-021-01394-0
Ozenen Kavlak, M., Cabuk, S. N., & Cetin, M. (2021). Development of forest fire risk map using geographical information systems and remote sensing capabilities: Ören case. Environmental Science and Pollution Research, 28 (25), 33265–33291. https://doi.org/10.1007/s11356-021-13080-9
Parajuli, A., Gautam, A. P., Sharma, S. P., Bhujel, K. B., Sharma, G., Thapa, P. B., Bist, B. S., & Poudel, S. (2020). Forest fire risk mapping using GIS and remote sensing in two major landscapes of Nepal. Geomatics, Natural Hazards and Risk, 11 (1), 2569–2586. https://doi.org/10.1080/19475705.2020.1853251
Paveglio, T. B., Kooistra, C., Hall, T., & Pickering, M. (2016). Understanding the effect of large wildfires on residents’ well-being: What factors influence wildfire impact? Forest Science, 62 (1), 59–69. https://doi.org/10.5849/forsci.15-021
Povak, N. A., Hessburg, P. F., & Salter, R. B. (2018). Evidence for scale‐dependent topographic controls on wildfire spread. Ecosphere , 9 (10). https://doi.org/10.1002/ecs2.2443
Pozo, R. A., Galleguillos, M., González, M. E., Vásquez, F., & Arriagada, R. (2022). Assessing the socio-economic and land-cover drivers of wildfire activity and its spatiotemporal distribution in south-central Chile. Science of the Total Environment, 810 , 152002. https://doi.org/10.1016/j.scitotenv.2021.152002
Prestemon, J. P., Pye, J. M., Butry, D. T., Holmes, T. P., & Mercer, D. E. (2002). Understanding broadscale wildfire risks in a human-dominated landscape. Forest Science, 48 (4), 685–693. https://doi.org/10.1093/forestscience/48.4.685
Ray, T., Malasiya, D., Verma, A., Purswani, E., Qureshi, A., Khan, M. L., & Verma, S. (2023). Characterization of spatial–temporal distribution of forest fire in Chhattisgarh, India, using MODIS-based active fire data. Sustainability , 15 (9), Article 9. https://doi.org/10.3390/su15097046
Reddy, C. S., Bird, N. G., Sreelakshmi, S., Manikandan, T. M., Asra, M., Krishna, P. H., Jha, C. S., Rao, P. V. N., & Diwakar, P. G. (2019). Identification and characterization of spatio-temporal hotspots of forest fires in South Asia. Environmental Monitoring and Assessment, 191 (S3), 791. https://doi.org/10.1007/s10661-019-7695-6
Rodrigues, M., Jiménez, A., & de la Riva, J. (2016). Analysis of recent spatial–temporal evolution of human driving factors of wildfires in Spain. Natural Hazards, 84 (3), 2049–2070. https://doi.org/10.1007/s11069-016-2533-4
Roshani, Sajjad, H., Rahaman, M. H., Rehman, S., Masroor, M., & Ahmed, R. (2022). Assessing forest health using remote sensing-based indicators and fuzzy analytic hierarchy process in Valmiki Tiger Reserve, India. International Journal of Environmental Science and Technology . https://doi.org/10.1007/s13762-022-04512-1
Roy, P. S. (2003). Forest fire and degradation assessment using satellite remote sensing and geographic information system. Satellite Remote Sensing and GIS Applications in Agricultural Meteorology, 361 , 400.
Saaty, T. L. (1980). The analytic hierarchy process . Mcgrawhill international.
Saaty, T. L. (2003). Decision-making with the AHP: Why is the principal eigenvector necessary. European Journal of Operational Research, 145 (1), 85–91. https://doi.org/10.1016/S0377-2217(02)00227-8
Saha, S. (2002). Anthropogenic fire regime in a deciduous forest of central India. Current Science , 1144–1147.
Salavati, G., Saniei, E., Ghaderpour, E., & Hassan, Q. K. (2022). Wildfire risk forecasting using weights of evidence and statistical index models. Sustainability , 14 (7), Article 7. https://doi.org/10.3390/su14073881
Santín, C., & Doerr, S. H. (2016). Fire effects on soils: The human dimension. Philosophical Transactions of the Royal Society B: Biological Sciences, 371 (1696), 20150171. https://doi.org/10.1098/rstb.2015.0171
Santos, S. M. B. dos, Bento-Gonçalves, A., Franca-Rocha, W., & Baptista, G. (2020). Assessment of Burned Forest Area Severity and Postfire Regrowth in Chapada Diamantina National Park (Bahia, Brazil) Using dNBR and RdNBR Spectral Indices. Geosciences , 10 (3), Article 3. https://doi.org/10.3390/geosciences10030106
Santos, F. L. M., Nogueira, J., Souza, R. A. F. D., Falleiro, R. M., Schmidt, I. B., & Libonati, R. (2021). Prescribed burning reduces large, high-intensity wildfires and emissions in the Brazilian Savanna. Fire, 4 (3), 56. https://doi.org/10.3390/fire4030056
Sari, F. (2023). Identifying anthropogenic and natural causes of wildfires by maximum entropy method-based ignition susceptibility distribution models. Journal of Forestry Research, 34 (2), 355–371. https://doi.org/10.1007/s11676-022-01502-4
Satendra, & Kaushik, A. D. (2014). Forest fire disaster management. National Institute of Disaster Management, Ministry of Home Affairs, New Delhi. https://nidm.gov.in/pdf/pubs/forest%20fire.pdf
Satir, O., Berberoglu, S., & Donmez, C. (2016). Mapping regional forest fire probability using artificial neural network model in a Mediterranean forest ecosystem. Geomatics, Natural Hazards and Risk, 7 (5), 1645–1658. https://doi.org/10.1080/19475705.2015.1084541
Schmerbeck, J., & Fiener, P. (2015). Wildfires, ecosystem services, and biodiversity in tropical dry forest in India. Environmental Management, 56 (2), 355–372. https://doi.org/10.1007/s00267-015-0502-4
Sen, P. K. (1968). Estimates of the regression coefficient based on Kendall’s Tau. Journal of the American Statistical Association, 63 (324), 1379–1389. https://doi.org/10.1080/01621459.1968.10480934
Silva, I. D. B., Valle, M. E., Barros, L. C., & Meyer, J. F. C. A. (2020). A wildfire warning system applied to the state of Acre in the Brazilian Amazon. Applied Soft Computing, 89 , 106075. https://doi.org/10.1016/j.asoc.2020.106075
Sivrikaya, F., & Küçük, Ö. (2022). Modeling forest fire risk based on GIS-based analytical hierarchy process and statistical analysis in Mediterranean region. Ecological Informatics, 68 , 101537. https://doi.org/10.1016/j.ecoinf.2021.101537
Sofan, P., Bruce, D., Schroeder, W., Jones, E., & Marsden, J. (2020). Assessment of VIIRS 375 m active fire using tropical peatland combustion algorithm applied to Landsat-8 over Indonesia’s peatlands. International Journal of Digital Earth, 13 (12), 1695–1716. https://doi.org/10.1080/17538947.2020.1791268
Srivastava, S. K., Saran, S., de By, R. A., & Dadhwal, V. K. (2014). A geo-information system approach for forest fire likelihood based on causative and anti-causative factors. International Journal of Geographical Information Science, 28 (3), 427–454. https://doi.org/10.1080/13658816.2013.797984
Stephenson, C., Handmer, J., & Betts, R. (2013). Estimating the economic, social and environmental impacts of wildfires in Australia. Environmental Hazards, 12 (2), 93–111.
Sunar, F., & Özkan, C. (2001). Forest fire analysis with remote sensing data. International Journal of Remote Sensing, 22 (12), 2265–2277. https://doi.org/10.1080/01431160118510
Surbhi Singh, S., & Jeganathan, C. (2024). Using ensemble machine learning algorithm to predict forest fire occurrence probability in Madhya Pradesh and Chhattisgarh. India. Advances in Space Research, 73 (6), 2969–2987. https://doi.org/10.1016/j.asr.2023.12.054
Suryabhagavan, K. V., Alemu, M., & Balakrishnan, M. (2016). GIS-based multi-criteria decision analysis for forest fire susceptibility mapping: A case study in Harenna forest, southwestern Ethiopia. Tropical Ecology, 57 (1), 33–43.
Tariq, A., Jiango, Y., Lu, L., Jamil, A., Al-ashkar, I., Kamran, M., & Sabagh, A. E. (2023). Integrated use of Sentinel-1 and Sentinel-2 data and open-source machine learning algorithms for burnt and unburnt scars. Geomatics, Natural Hazards and Risk, 14 (1), 2190856. https://doi.org/10.1080/19475705.2023.2190856
Tiwari, A., Shoab, M., & Dixit, A. (2021). GIS-based forest fire susceptibility modeling in Pauri Garhwal, India: A comparative assessment of frequency ratio, analytic hierarchy process and fuzzy modeling techniques. Natural Hazards, 105 (2), 1189–1230. https://doi.org/10.1007/s11069-020-04351-8
Tyukavina, A., Potapov, P., Hansen, M. C., Pickens, A. H., Stehman, S. V., Turubanova, S., Parker, D., Zalles, V., Lima, A., Kommareddy, I., Song, X.-P., Wang, L., & Harris, N. (2022). Global trends of forest loss due to fire from 2001 to 2019. Frontiers in Remote Sensing, 3 , 825190. https://doi.org/10.3389/frsen.2022.825190
Vadrevu, K., Eaturu, A., & Badarinath, K. (2009). Fire risk evaluation using multicriteria analysis—A case study. Environmental Monitoring and Assessment, 166 , 223–239. https://doi.org/10.1007/s10661-009-0997-3
Vadrevu, K. P., Csiszar, I., Ellicott, E., Giglio, L., Badarinath, K. V. S., Vermote, E., & Justice, C. (2013). Hotspot analysis of vegetation fires and intensity in the Indian Region. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 6 (1), 224–238. https://doi.org/10.1109/JSTARS.2012.2210699
Vadrevu, K. P., Lasko, K., Giglio, L., Schroeder, W., Biswas, S., & Justice, C. (2019). Trends in vegetation fires in South and Southeast Asian Countries. Scientific Reports, 9 (1), 7422. https://doi.org/10.1038/s41598-019-43940-x
van der Werf, G. R., Randerson, J. T., Giglio, L., Gobron, N., & Dolman, A. J. (2008). Climate controls on the variability of fires in the tropics and subtropics. Global Biogeochemical Cycles , 22 (3). https://doi.org/10.1029/2007GB003122
Van Hoang, T., Chou, T. Y., Fang, Y. M., Nguyen, N. T., Nguyen, Q. H., Xuan Canh, P., Ngo Bao Toan, D., Nguyen, X. L., & Meadows, M. E. (2020). Mapping Forest Fire Risk and Development of Early Warning System for NW Vietnam Using AHP and MCA/GIS Methods. Applied Sciences , 10 (12), 4348. https://doi.org/10.3390/app10124348
Whitman, E., Sherren, K., & Rapaport, E. (2015). Increasing daily wildfire risk in the Acadian Forest Region of Nova Scotia, Canada, under future climate change. Regional Environmental Change, 15 (7), 1447–1459. https://doi.org/10.1007/s10113-014-0698-5
Zeren Cetin, I., Ozel, H. B., & Varol, T. (2020). Integrating of settlement area in urban and forest area of Bartin with climatic condition decision for managements. Air Quality, Atmosphere & Health, 13 (8), 1013–1022. https://doi.org/10.1007/s11869-020-00871-1
Zeren Cetin, I., Varol, T., & Ozel, H. B. (2023a). A geographic information systems and remote sensing–based approach to assess urban micro-climate change and its impact on human health in Bartin. Turkey. Environmental Monitoring and Assessment, 195 (5), 540. https://doi.org/10.1007/s10661-023-11105-z
Zeren Cetin, I., Varol, T., Ozel, H. B., & Sevik, H. (2023b). The effects of climate on land use/cover: A case study in Turkey by using remote sensing data. Environmental Science and Pollution Research, 30 (3), 5688–5699. https://doi.org/10.1007/s11356-022-22566-z
Zhang, Z., Feng, Z., Zhang, H., Zhao, J., Yu, S., Du, W., Zhang, Z., Feng, Z., Zhang, H., Zhao, J., Yu, S., & Du, W. (2017). Spatial distribution of grassland fires at the regional scale based on the MODIS active fire products. International Journal of Wildland Fire, 26 (3), 209–218. https://doi.org/10.1071/WF16026
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The authors are thankful to Madhya Pradesh Forest Department for proving the essential data about the study area and Indian Institute of Remote Sensing (IIRS) Dehradun for providing free access GIS data. We are also thankful to Ms. Shailja Mamgain and Mr. Prince from the Disaster Management Studies Lab at IIRS for their valuable technical support in the realm of GIS software assistance. Futher, we extend our gratitude to Ms. Monika for her review of the manuscript, focusing on both the English language and writing style.
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Communications Earth & Environment volume 5 , Article number: 465 ( 2024 ) Cite this article
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On 25 April 2015, the Gorkha earthquake triggered a large rock-ice avalanche and an air blast disaster in the Langtang Valley, Nepal. More than 350 people were killed or left missing. Here we reconstruct the evolution of the Langtang avalanche-air blast using field investigations and numerical modeling and examine the influence of two primary climate-related phenomena: snowfall anomalies and warm temperatures. Our findings suggest a deep snow cover fosters the formation of a dispersed avalanche, which increases the mobility and destructive power of the powder cloud air blast. Elevated air temperatures intensify meltwater production and lubricate the flowing mass. Both mechanisms contributed to the Langtang disaster. Our study underscores the essential impact of snow cover and air temperature on the risk assessment of high-altitude rock-ice avalanches, highlighting how seasonal and climatic variations affect avalanche runout and air blast dynamics.
Large rock-ice avalanches are geophysical mass flows composed of a mixture of rock and ice. They can be extremely hazardous due to their extremely high velocity and long runout 1 , 2 , 3 . In earthquake-prone regions globally changing climate appears to be exacerbating these hazards 4 . Scientists have long recognized rapid global climate change favors the instability of mountains in glacial and periglacial areas 5 , 6 , 7 . Nevertheless, to our knowledge, no hazard risk assessment considers how the impact of climate change contributes to their destructive potential, especially in terms of runout and flow regime transitions, such as the formation of hazardous air blasts.
One phenomenon of climate change is frequent snowfall anomalies in high-altitude regions. In the past decades, the duration of snowfall decreased, while snowfall intensity showed an increasing trend 8 , 9 , 10 . The thick snow cover arising from snowfall anomalies is an important mass source of the avalanche core. This snow entrainment process amplifies the avalanche volume 11 , 12 , lubricates the avalanche movement 13 , and exacerbates the formation of a rock-ice-snow powder avalanche 14 . This type of avalanche often generates powerful air blasts capable of causing damage and human fatalities far beyond the reach of avalanche core 15 .
Another feature of the ongoing climate change problem is warming 16 , 17 , moreover, how changing snow and air temperatures will change avalanche flow dynamics. In existing rock-ice avalanche models, the sliding mass is treated as a thermally insulated system, ignoring the effect of ambient environment 18 , 19 . Frictional shearing 20 , entrainment process 13 , and particle collisions 21 are heat energy sources that change the avalanche temperature and produce meltwater. It is important to note that avalanche snow (ice) exists near its melting point and frictional heating can easily supply the necessary energy input needed to produce meltwater. The porous-medium structure of avalanches and the dispersive movement of granular particles allow the intake and outburst of ambient air 14 . This interaction with the ambient environment is inevitable during avalanche movement and can either enhance or hinder the heating process. The temperature difference between the avalanche and ambient air leads to a heat exchange that greatly influences meltwater production and the flow regime of the avalanche core.
One striking example is the rock-ice avalanche of Langtang (2015), which was triggered by the Gorkha earthquake in a warm season, releasing several ice masses well above the snowline 22 . The thick snow cover amplified the avalanche volume and formed a rock-ice-snow powder avalanche. Fujita et al. 23 attributed the massive destruction caused by the avalanche directly to a snow cover anomaly. The air blast nearly destroyed the Langtang village and flattened a forest on the valley counter-slope 24 .
In this paper, we reconstruct the evolution of the Langtang avalanche and generated air blasts based on documented field measurements and numerical modeling. We further conduct simulations with different snow cover depths and air temperatures to investigate the impact of snow entrainment and ambient environment, indicating how seasonal and climatic influences may affect the danger of rock-ice avalanches. The study focuses exclusively on changes in runout and flow regimes under different snow cover and air temperature conditions, rather than variability in avalanche occurrence due to climate change. Our primary goal is to quantify the danger arising from rock-ice-snow avalanches, containing both a dense flow core and dust cloud, in different mountain conditions that can be eventually associated with changing climate scenarios.
On 25 April 2015, the Gorkha earthquake (Mw7.9) triggered a large rock-ice avalanche in the Langtang Valley, Nepal. Details of the Langtang avalanche are well recorded in existing literature. Thus, here we briefly introduce the essential information concerning this disastrous event. The avalanche was initiated as a multi-source ice avalanche (initiated in several release areas) of ~3.5 × 10 6 m 3 , and the release areas are located over 6000 m a.s.l. (Fig. 1a, b ). Satellite images (April–May 2015) indicated an evident snowline at 4000–4500 m a.s.l. Four anomalous snowfall events occurred during the previous winter (October 2014–April 25, 2015), resulting in a thick snow cover on the mountain surface 23 . Field investigation reveals that the released ice mass entrained snow (over 4500 m a.s.l.) and debris cover (below 4500 m a.s.l.) along the travel path (Fig. 1c ) 23 . According to pre- and post-event digital surface models 25 , we knew that the avalanche involved a total volume of 14.38 × 10 6 m 3 of rock, ice, and snow mass. Of this, a total of 6.95 × 10 6 m 3 accumulated in the Langtang Valley 25 . The Langtang village is located on the valley floor (Fig. 1d, e ) and was not struck directly by the avalanche core. The air blast generated by the avalanche destroyed large parts of the village and caused over 350 deaths. This is confirmed by field observations showing that many houses constructed of stone slabs were flattened or destroyed by the air blast 24 (Supplementary Fig. 1a ). Furthermore, the air blast impacted an area of 1 km up and down the valley and flattened a forest on the opposite mountain (Fig. 1e , Supplementary Fig. 1b ), as described by Kargel et al. 22 .
a The release area from Langtang Lirung. The size of released materials helps estimate the initial volume. b The direction from where additional ice was released from around Langtang II. Both are shown in detail in the right part of the figure. c The plateau where the rock entrainment occurred. d The headwall above the village (height ~500 m). e Shows the view angle of the photo as an inset where destroyed houses ( e1 ), blown-over trees ( e2 ), and deposited ice–debris mix on the far side of the valley ( e3 ) are shown. Images taken from the helicopter by D.F. Breashears/GlacierWorks.
Two local meteorological stations record the air temperature: Kyanjing station at 3862 m a.s.l. (6.3 km away from the Langtang village) and Yala Base camp station at 5058 m a.s.l. (10.2 km from the Langtang village) 26 . The average measured temperature on 25 April was −0.65 to 9.05 °C at Kyanjing station (2012–2014, 2016–2018) and −8.10 to 0.18 °C at Yala Base camp station (2013, 2016–2018). Another pluviometer at 4831 m a.s.l. recorded an air temperature of −0.4° to 3.6° within 30 min before the avalanche occurred, indicating a warm environment 23 . The Gorkha earthquake occurred at 11:56 Nepal Standard Time, therefore a high temperature (9 and 0 °C at 3862 and 5058 m a.s.l., arising from the recorded max value) is applied for the following analysis, indicating an air temperature gradient of ~0.75 °C per 100 m elevation difference. According to Fujita et al. 23 , the snow depth at Yala station was ~1.5 m. Using this snow depth value, combined with the location of the snow line, we derived a preliminary estimate of the snow cover gradient. Based on this estimate, the snow depth at the release area was calibrated, ensuring that the entrained and total avalanche volumes match the measured data.
Modeling results of the Langtang avalanche are presented in Fig. 2 . The snow depth at the release area is estimated to be 3 m, and a gradient of −0.15 m per 100 m is determined with this depth value and the location of the snow line. The modeled released ice volume is 3.65 × 10 6 m 3 , and the sliding mass entrained snow and rock materials of 11.20 × 10 6 m 3 during the movement process (simulated total volume of 14.85 × 10 6 m 3 ). The error between the simulated and actual volumes (initial volume of 3.50 × 10 6 and total volume of 14.38 × 10 6 m 3 ) is within 5%. Two main deposit areas are observed in the simulation: the platform at 4500 m a.s.l. and the Langtang Valley (Fig. 2a ). The depth of deposits in the Langtang Valley is over 30 m, as observed by Fujita et al. 23 . The simulated avalanche volume and the deposit area match these observations. The calculated avalanche core reached the maximum velocity of over 90 m s −1 at 5000–5500 m a.s.l. When the avalanche passed the Langtang Valley, immediately before hitting the toe of the opposite mountain, it was traveling at 57 m s −1 (Fig. 2b ), matching the velocity estimated by the run-up equation (63 m s −1 , Kargel et al. 22 ).
a Final deposit distribution of the avalanche core, matching the observations (red lines). b Maximum velocity of the avalanche core. c Maximum mean pressure of the air blast. d and e Powder pressure profile at the Langtang village (point A in c ) and the forest at the mountain toe (point B in c ). The satellite image arises from Planet (Images ©2021 Planet Labs PBC).
Figure 2c shows the dynamic pressure of the Langtang avalanche-induced air blast. The air blast shows an impact area far beyond the avalanche core, covering the whole Langtang village and the forest on the opposite mountainside. In the Langtang village, the dynamic pressure of the air blast exceeds 15 kPa but decreases gradually to 6 kPa as it moves over the village (a rule of thumb used by avalanche engineers is that a 1 kPa air blast will violently blow a human to the ground at impact). The turbulent fluctuations greatly magnify the air blast pressure. At a specific location (simulation point) near Langtang village (point A in Fig. 2c ), the maximum pressure reaches 28 kPa (Fig. 2d ), nearly double the pressure arising from the mean velocity. Such high pressures are capable of destroying houses, as observed. On the opposite mountain slope, the pressure of the air blast reaches a mean of 10 kPa and a maximum of 18 kPa at the mountain toe (Fig. 2e ) but decreases substantially as it climbs up the mountain. Tree-breakage calculations follow the method proposed by Feistl et al. 27 . Trees on the opposite mountain face are Abies and Rhododendron species with an average diameter of 0.16 m 23 . Using a bending strength of 72 MPa, modeling results indicate a tree-breakage area of about 0.8 km 2 , extending 1 km up and down the valley from the deposit center and 550 m up the mountain (Fig. 2c ). The calculated tree-breakage area essentially matches the observations 22 .
We set up scenarios to investigate the impact of snow cover on the dynamics of rock-ice avalanches and air blasts. The snow cover at the release area is set at 0–3 m in depth with a constant gradient of −0.15 m per 100 m. The air temperature remains fixed. In the RAMMS model, the snow cover is adjusted based on the slope angle and curvature along with the elevation gradient to produce a realistic snow distribution on mountainous terrain. Snow cover distributions are shown in Fig. 3a–d .
a – d Snow cover distribution in different scenarios. Red dotted line represents the calculated domain. e – h Impacts of snow cover on the avalanche extent. i – l Impacts of snow cover on the air blast dynamics. m – p Pressure profile at the Langtang village (Point A in i ) in cases of different snow covers. The satellite image arises from Planet (Images ©2021 Planet Labs PBC).
Modeling results indicate a longer runout distance and higher mobility in the case of a thick snow cover (Fig. 3e–h ). When the snow cover at the release area reaches 3 m, which corresponds to the modeling results in Fig. 2 , the calculated avalanche dynamics match the observed conditions well. In the case without considering snow entrainment (snow cover = 0 m), the rock-ice avalanche stops before hitting the opposite mountain. The sliding mass primarily deposits at the 4500 m a.s.l. platform, with only a little mass reaching the Langtang Valley. For the air blast hazards, the cloud dynamics are again related to the thickness of the snow cover. Both the impact area and dynamic pressure of the air blast decrease in the case of a thin snow cover (Fig. 3i–p ). When there is no snow cover, the mean dynamic pressure at the Langtang village is only 2.5 kPa, and only a few trees are damaged on the opposite mountain (Fig. 3l, p ), showing minor destruction compared with the actual event. This implies that the entrained snow facilitates the formation of a dispersed powder avalanche and is a primary factor that led to the Langtang disaster. Our numerical results strongly support the hypothesis of Fujita et al. 23 .
Further scenarios of different air temperatures are designed to investigate the impact of temperature variation on the danger arising from rock-ice avalanches, as presented in Fig. 4 . The air temperature at 3862 m a.s.l. (Kyanjing meteorological station) is set −1 to 19 °C with a constant gradient of 0.75 °C per 100 m. Here the snow cover depth remains fixed. Modeling results indicate that the avalanche core shows higher mobility in the case of a warm environment. When the air temperature at 3862 m a.s.l. reaches −1 °C, the heat transfer with the cold air restricts the melting of snow and ice. The meltwater is 74,000 t at the end of the event (Fig. 4g ), and the maximum water content in the avalanche core is ~600 mm m −3 (Fig. 4d ). In this scenario, relatively small amounts of material deposit in the Langtang Valley (Fig. 4a ) compared with the actual conditions. When the air temperature is 19 °C at 3862 m a.s.l., a warm environment, the produced meltwater reaches 170,000 t (Fig. 4i ), more than twice the amount calculated for a cold environment. The maximum water content in the avalanche core reaches over 1800 mm m −3 (Fig. 4f ), a high value. The rheological relationship applied here is an ever-decreasing Coulomb friction resistance with increasing water content 13 :
where \({\mu }_{\Phi }\) is the dry friction coefficient, \({\mu }_{\min }\) is the fully lubricated friction coefficient, representing the lowest friction, \({m}_{{\rm {w}}}\) is the water height in the flow and \({m}_{0}\) is the reference height. The friction decreases from \({\mu }_{\Phi }\) (dry avalanche) to \({\mu }_{\min }\) (fully lubricated flow) with the increase in water content. In the case of a warm environment (Fig. 4f ), the abundant amount of meltwater at the avalanche front provides lubrication (decreases the friction, Supplementary Fig. 2 ) leading to a fluid-like flow regime in the Langtang Valley and thus a long runout distance (Fig. 4c ). The avalanche moved over 1.5 km downstream of the Langtang Valley. For the Langtang avalanche, due to the low temperature of the released materials, the meltwater appears at ~20 s after the avalanche initiation and accumulates in the frontal lobe of the avalanche deposits (Fig. 4e, h ).
a – c Impacts of air temperature on the avalanche extent. d – f Impacts of air temperature on the water content distribution within the avalanche core. g – i Impacts of air temperature on meltwater production. Here, the air temperature is set as −1, 9, and 19 °C at 3862 m a.s.l. with a constant temperature gradient. The satellite image arises from Planet (Images ©2021 Planet Labs PBC).
Scientists suggest that ongoing climate change favors the initiation of rock-ice avalanches, but its impacts on avalanche formation and flow are rarely quantified 3 , 6 , 28 . With this purpose, using the Langtang avalanche, we numerically investigate two important phenomena arising from climate change to the destructive potential of rock-ice avalanches: snowfall anomalies and global warming.
For a rock-ice avalanche, snowfall anomalies will exacerbate the avalanche mobility and lead to an air blast problem. Anomalous snowfall and the associated thick snow cover favor snow entrainment in the mountain environment. This process can magnify the avalanche volume and change the flow behavior. Compared with ice and rock mass, snow is easily entrained because of the low shear stress threshold 29 . Snow is a material of low friction and can decrease the equivalent Coulomb frictional coefficient (in Eq. ( 13 )) of the avalanche core. One primary consequence of the snow entrainment is the increment of flow height, which increases the normal and shear stress acting on the ground surface. Combined with the entrainment process 12 , the additional shearing work attributable to the shear stress increment exacerbates the heat energy production within the avalanche core, therefore favoring meltwater production. The lubrication effect of the meltwater greatly enhances the avalanche mobility. Furthermore, the flowing resistance is a function of fluctuation energy \({R}_{\Phi }\) (Eq. ( 13 )), again related to the shearing work and the flow height. Chute experiments 30 indicate that friction decreases in proportion to the increase in the gravitational work rate or the shearing work rate. Without considering the entrainment process, there is no mass source for avalanches in motion. For a finite-sized avalanche, shear gradients within the avalanche core cause the flow height to decrease. The shearing work rate and production of fluctuation energy subsequently decline, and friction increases. The avalanche begins to starve and decelerate, eventually stopping on the slope.
As for the air blast hazard, the process of snow entrainment facilitates the formation of a rock–ice–snow avalanche with a dense granular core consisting of rock and ice fragments and a dust cloud of suspendable particles. The initial mass and momentum of the air blast are known to arise from the air movements caused by displacing air in the avalanche core 14 . The entrained snow is, therefore, an important mass/momentum source to transfer mass and momentum to the powder cloud, magnifying its impact area and dynamic pressure. In the case without snow entrainment, the Langtang avalanche-induced air blast hardly destroys the Langtang village and the forest (Fig. 3l ), principally different from the actual conditions. This implies air blast hazards could show a higher destructive force after an intense snowfall event. We suggest the previous snowfall anomalies and the snow entrainment were a primary factor that caused the Langtang disaster.
For rock-ice avalanches, the generation of heat energy and the phase change processes are of paramount interest due to the unique properties of ice and snow 18 , 31 . The components of snow and ice reside close to their melting points, and the frictional heat generated during the avalanche propels these materials toward a phase transition. This process is tempered by the ambient air temperature. Recorded videos 3 and our detailed investigations into avalanche evolution provide compelling evidence of the physical interaction between the avalanche core and the ambient air temperature. The avalanche core entrains the ambient air during the movement process and outbursts the dust-mixed air to generate the powder cloud. The Reynolds number of natural rock-ice avalanches 32 reaches 10 4 −10 6 . Such a turbulent structure facilitates the mixture of the granular particles and entrained air, therefore exacerbating a heat exchange between the avalanche core with the ambient environment. Our modeling results of the Langtang avalanche suggest a warm air temperature amplifies the meltwater production and lubricates the flowing mass.
For simplification and engineering applications, we used an experimentally based heat transfer relationship for sphere particles 33 . Though the impacts of particle shape and porosity are ignored, this relationship is sensitive to the particle size. More precisely, the particle surface area. According to the heat transfer relationship (Eq. ( 12 )):
The heat transfer is proportional to r −1.5 – r −2.0 . In this study, due to the lack of accurate particle size distribution, particle sizes for snow (7 cm), ice (10 cm), and rock (30 cm) are determined based on our practical experience with numerous historical avalanches and the existing literature 34 , 35 . This implies heat energy exchange between snow particles with air reaches 8.9–18.4 times rock particles of the same volume. For the Langtang avalanche, the volume of the entrained snow accounts for >70% of the total volume 23 . The process from avalanche initiation to deposition lasts ~3 min, and the air temperature in the Langtang Valley reaches ~14 °C. The small-sized snow particles, prolonged movement, and warm air temperature intensify the heat exchange and meltwater production, resulting in a flow-like movement in the Langtang Valley. Sensitivity analysis indicates a longer runout distance, more meltwater production, and a highly fluid flow regime of avalanches in a warm environment. The impacts of heat transfer with the ambient air on meltwater production and avalanche runout can be even higher than the contribution of snowpack temperature (see extra simulations presented in Supplementary Fig. 3 ).
Notably, the Gorkha earthquake and Langtang avalanche occurred at noon, in a warm environment. If the avalanche occurs at night, a cold environment hinders the meltwater production and leads to a smaller runout and impact area that is similar to the scenario depicted in Fig. 4a . We are not able to predict when a catastrophic earthquake will occur, but our analysis of air temperature impacts indicates that the destructive potential of rock-ice avalanches is not only related to large-scale global warming but also to short-term diurnal temperature.
Risk assessments of rock-ice avalanches are a primary concern in high-altitude mountainous regions. Confronted with the problem of extreme and rare events and the lack of historical documentation, avalanche dynamics modeling will play a key role in assessing the safety of settlements, transportation routes, and hiking trails. To our knowledge, the impacts of climate change on the destructive potential of rock–ice avalanches are multifaceted, but rarely considered. We suggest the snowfall anomalies and warm air temperature greatly contributed to the Langtang disaster.
At noon on April 25, 2015, the Mw 7.9 Gorkha earthquake precipitated a large rock–ice avalanche in the Langtang Valley. The resultant air blasts obliterated the Langtang village, a nearby forest, and led to the tragic loss of over 350 lives. Through meticulous field investigations and advanced numerical modeling, we have identified two principal factors contributing to the severity of the Langtang disaster: anomalous snowfall and elevated temperatures. The substantial snow cover facilitated snow entrainment, promoting the development of a dispersed powder avalanche. This entrained snow significantly increased the avalanche volume, acted as a lubricant for the flowing mass, and amplified the destructive power of the air blast. Furthermore, the warm air temperature, in conjunction with the turbulent structure of the avalanche core, intensified heat exchange between the granular particles and the entrained air. This thermal process enhanced meltwater production, consequently altering the avalanche’s mobility. These mechanisms were crucial in intensifying the Langtang disaster. We emphasize the critical finding that incorporating the effects of snow cover and air temperature factors heavily influenced by seasonal and climatic changes—is essential when performing hazard analyses for high-altitude rock-ice avalanches. Our results reveal the inherent fragility of natural systems, particularly the mobility and destructive potential of rock-ice avalanches. Minor variations in temporal factors, climatic conditions, or the antecedent state of an event can either intensify or mitigate disastrous outcomes. This insight compels us to ponder how many disasters have been averted or caused by seemingly insignificant changes in the natural environment.
General framework.
We apply a depth-averaged model to simulate the flow dynamics of the rock-ice avalanche and the generated air blast 19 , 36 . The avalanche core Φ and the air blast Π are described by two distinct depth-averaged layers. The core layer comprises a granular ensemble of rock, ice, and snow particles capable of dispersion and compression, changing the interstitial air space of the core. The core movement is strongly influenced by the surface terrain and allows for both air intake and outburst. During the outburst process, the avalanche core transmits mass and momentum to the cloud Π and creates a turbulent structure in the cloud 14 . The cloud is, therefore, modeled as a turbulent flow, including suspensions of ice and rock dust that are transferred from the avalanche core. The governing equations for both the avalanche core and dust cloud are solved using well-established finite volume schemes within the software rapid mass movement simulation (RAMMS) 36 .
Here we follow the avalanche core model 19 , 36 . The model involves some essential processes of an avalanche flow, including entrainment of path materials 37 and meltwater production 19 . In the model, the movement of the avalanche core Φ is described by three state valuables: the so-called co-volume height \({\hat{h}}_{\Phi }\) , the dispersed or flowing height \({h}_{\Phi }\) and the depth-averaged velocity \({\vec{u}}_{\Phi }\) that parallel to the slope surface. The co-volume represents the densest packing of ice/rock granules found in the deposit area, corresponding to a co-volume density \({\hat{\rho }}_{\Phi }\) . Because the avalanche core is a multiphase flow of mixed components, the co-volume height \({\hat{h}}_{\Phi }\) is defined as
where \({\rho }_{{\rm {i}}}\) , \({\rho }_{{\rm {s}}}\) , \({\rho }_{{\rm {r}}}\) , \({\rho }_{{\rm {w}}}\) , \({\hat{h}}_{{{\rm{i}}}}\) , \({\hat{h}}_{{{\rm{s}}}}\) , \({\hat{h}}_{{{\rm{r}}}}\) , \({\hat{h}}_{{{\rm{w}}}}\) are the material density and co-volume height of ice, snow, rock, and water, respectively. The model assumes both constant density and velocity profiles of each material. The primary governing equations are as follows:
Equations ( 4 ) and ( 7 ) represent the mass and momentum balances of the avalanche core, which involves the avalanche entrainment \({\dot{M}}_{\Sigma \to \Phi }\) and mass/momentum transfer to the cloud \({\dot{M}}_{\Phi \to \Pi }\) . Equation ( 5 ) describes the dispersive movement of the avalanche core. The term \({\mathbb{D}}(t,{k}_{z},{\dot{k}}_{z},{\ddot{k}}_{z})\) represents the variation of core height due to dispersive pressure effects; we employ the model presented in Buser and Bartelt 38 . Equation ( 6 ) is the mass balance of each phase in the core, including rock, ice, snow, and water. The mass change of each phase arises from the entrainment process, air blast initiation, and phase change. Equations ( 8 ) and ( 9 ) show the balance of fluctuation energy and heat energy. Equation ( 10 ) describes the production and transport of meltwater in the avalanche core. The meltwater arises from both the ice melting and snow melting. The model assumes the mean core temperature \({T}_{\Phi }\) never exceeds the melting temperature of \({T}_{{\rm {m}}}\) until all the ice and snow melt. The heat energy applied for meltwater production is presented in Eq. ( 11 ). The parameters included in Eqs. ( 4 )–( 11 ) are well described by Bartelt et al. 19 and Munch et al. 39 and are listed in Table 1 .
In the heat energy balance of Eq. ( 9 ), the heat transfer from avalanche to the ambient, entrained air is newly involved, defined as
where \({A}_{{{\rm{s}}}}=n\pi {r}^{2}\) , \(n=\frac{{3\rho }_{\Phi }{h}_{\Phi }A}{4{\rho }_{g}\pi {r}^{3}}\) is the particle number, \({\rho }_{{{\rm{g}}}}\) is the particle density, r is the particle radius, \({T}_{\Phi }-{T}_{\Lambda }\) represents the temperature difference between the avalanche core \({T}_{\Phi }\) and the ambient air \({T}_{\Lambda }\) . \(H=\frac{{{{\rm{Nu}}}}\cdot {k}_{{{\rm{a}}}}}{2r}\) is the experimentally based heat transfer coefficient 33 , \({k}_{{{\rm{a}}}}=\) 0.0257 W m −1 K −1 is the thermal conductivity, \({{{Nu}}}=2+0.6{{\mathrm{Re}}}^{\frac{1}{2}}{\Pr }^{\frac{1}{3}}\) is the dimensionless Nusselt number, \({Re}=\frac{2{ur}}{{\nu }_{{{\rm{a}}}}}\) is the Reynolds number, \(Pr =\frac{{c}_{{{\rm{a}}}}{\nu }_{{{\rm{a}}}}}{{k}_{{{\rm{a}}}}}\) is the Prandtl number of the air, \({c}_{{{\rm{a}}}}\) is the specific heat capacity of the air.
A fundamental feature of the avalanche core model is the partitioning of a primary dissipative process, shearing, into the production of heat \({E}_{\Phi }\) (internal energy) and non-directional kinetic energy \({R}_{\Phi }\) (granular temperature). The work done by shearing \({\dot{W}}_{\Phi }={S}_{\Phi }{{\rm{||}}}{\vec{u}}_{\Phi }{{\rm{||}}}\) is divided into microscopic and macroscopic random energy (heat and granular fluctuations) by parameter \({\alpha }_{\Phi }\) 38 . Shearing is controlled by the process-based Voellmy-type rheology 40 :
where ( \({\mu }_{\Phi }\) , \({\xi }_{\Phi }\) ) are the Coulomb and turbulent friction coefficients, respectively, defined as functions of the fluctuation energy \({R}_{\Phi }\) , temperature \({T}_{\Phi }\) and water content \({m}_{{{\rm{w}}}}\) . The flow friction \({S}_{\Phi }\) is dependent on the dispersive properties of the random energy \({R}_{\Phi }\) , avalanche mobility, and, therefore, the formation of the powder cloud is strongly influenced by the shearing process.
A similar set of partial differential equations is proposed to describe the movement of the powder cloud Π. To track the mass changes of different materials in the cloud, an improvement of the model is to suggest the powder cloud as a mixture of a rock powder cloud \({\Pi }_{{{\rm{r}}}}\) and an ice powder cloud \({\Pi }_{{\rm{{i}}}}\) . Therefore, the cloud density depends on the volumetric ratio of rock and ice within the cloud. We begin by presenting the mass balance equations:
Equations ( 14 ) and ( 15 ) represent the mass balance of the rock powder cloud \({\Pi }_{{{\rm{r}}}}\) and ice powder cloud \({\Pi }_{{{\rm{i}}}}\) , respectively, and Eq. ( 16 ) described the mass balance of the total powder cloud Π. Similar to the core, ( \({\hat{h}}_{\Pi {{\rm{r}}}}\) , \({\hat{h}}_{\Pi {{\rm{i}}}}\) , \({\hat{h}}_{\Pi }\) ) represents the initial height of \({\Pi }_{{{\rm{r}}}}\) , \({\Pi }_{{{\rm{i}}}}\) and Π, respectively, and are given by the initial cloud density ( \({\hat{\rho }}_{\Pi {{\rm{r}}}}\) , \({\hat{\rho }}_{\Pi {{\rm{i}}}}\) and \({\hat{\rho }}_{\Pi }\) ) before blowing out from the avalanche core \(\Phi\) . The true cloud height \({h}_{\Pi }\) is affected by clouds ejected from the core ( \({\dot{M}}_{\Phi \to \Pi {{\rm{r}}}}\) , \({\dot{M}}_{\Phi \to \Pi {{\rm{i}}}}\) ) and ambient air entrainment \({\dot{M}}_{\Lambda \to \Pi }\) . Due to this air entrainment, the cloud height increases during the propagation process and the density decreases to \({\rho }_{\Pi }\) , satisfying \({\rho }_{\Pi }={\rho }_{{{\rm{i}}}}\frac{{\nu }_{i}{\hat{h}}_{\Pi {{\rm{i}}}}}{{h}_{\Pi }+{\nu }_{i}{\hat{h}}_{\Pi {{\rm{i}}}}+{\nu }_{r}{\hat{h}}_{\Pi {{\rm{r}}}}}+{\rho }_{{{\rm{r}}}}\frac{{\nu }_{r}{\hat{h}}_{\Pi {{\rm{r}}}}}{{h}_{\Pi }+{\nu }_{i}{\hat{h}}_{\Pi {{\rm{i}}}}+{\nu }_{r}{\hat{h}}_{\Pi {{\rm{r}}}}}+{\rho }_{\Lambda }\frac{{h}_{\Pi }}{{h}_{\Pi }+{\nu }_{i}{\hat{h}}_{\Pi {{\rm{i}}}}+{\nu }_{r}{\hat{h}}_{\Pi {{\rm{r}}}}}\) , \({\rho }_{{{\rm{i}}}}\) = 971 kg m −3 is the ice density, \({\rho }_{{{\rm{r}}}}\) = 2500 kg m −3 is the rock density, \({\rho }_{\Lambda }\) = 1.225 kg m −3 is the air density ( \({\nu }_{{{\rm{i}}}}=\frac{{\hat{\rho }}_{\Pi {{\rm{i}}}}-{\rho }_{\Lambda }}{{\rho }_{{{\rm{i}}}}-{\rho }_{\Lambda }}\) , \({\nu }_{{{\rm{r}}}}\) = \(\frac{{\hat{\rho }}_{\Pi {{\rm{r}}}}-{\rho }_{\Lambda }}{{\rho }_{{{\rm{r}}}}-{\rho }_{\Lambda }}\) ) represents the solid fraction in the initial ice and rock powder cloud.
The momentum balance of the powder cloud is
The mixed ice/rock powder cloud moves with a mean velocity vector \({\vec{u}}_{\Pi }\) . The cloud is driven by the initial momentum transferred from the avalanche core \({\dot{M}}_{\Phi \to \Pi }{\vec{u}}_{\Phi }\) and the gravity \(\frac{\left({\rho }_{\Pi }-{\rho }_{\Lambda }\right)}{{\rho }_{\Pi }}\vec{G}\) .
Another important improvement of the proposed model is the inclusion of turbulence. The instantaneous air blast velocity \({\widetilde{u}}_{\Pi }\) is written as the sum of a mean \({\vec{u}}_{\Pi }\) and a fluctuating component \({\vec{u}{\prime} }_{\Pi }\) . The energy associated with the fluctuation of the granules \({R}_{\Pi }\left(x,y,z,t\right)\) can be written as 41
The fluctuation energy is divided into three orthogonal components in the x , y , z directions. Here the velocity fluctuation is assumed to be isotropic, and thus \({R}_{\Pi ,x}={R}_{\Pi ,y}={R}_{\Pi ,z}=\frac{1}{3}{R}_{\Pi }\) . The balance equation of the fluctuation energy can be written as:
We suggest the fluctuation energy has three sources: fluctuation energy that is created in the avalanche core and transported to the cloud \({\dot{M}}_{\Phi \to \Pi }{R}_{\Phi }\) , internal shearing \({\dot{W}}_{\Pi }=\left[{S}_{\Pi }\right]{{\rm{||}}}{\vec{u}}_{\Pi }{{\rm{||}}}\) and air entrainment \(\frac{1}{2}{\rho }_{\Lambda }{\dot{M}}_{\Lambda \to \Pi }{u}_{\Pi }^{2}\) . The fluctuation energy \({R}_{\Pi }\) of the cloud has a short lifetime and its dissipation is controlled by a decay coefficient \({\beta }_{\Pi }\) 15 .
In the air blast model, the air entrainment \({\dot{M}}_{\Lambda \to \Pi }\) and drag resistance \({S}_{\Pi }\) are defined as a contribution of both laminar and turbulent parts. Air entrainment is suggested as a function of the turbulent velocity 42 , 43 , the square root of the turbulent energy \({R}_{\Pi }\) : \({\dot{M}}_{\Lambda \to \Pi }={\alpha }_{{{\rm{L}}}}\left({\rho }_{\Pi }-{\rho }_{\Lambda }\right)+{\alpha }_{{{\rm{T}}}}\sqrt{{R}_{\Pi }{\hat{h}}_{\Pi }}\left({\rho }_{\Pi }-{\rho }_{\Lambda }\right)\) . The drag resistance is suggested as a direct function of the average velocity and turbulent energy: \({S}_{\Pi }={\rho }_{\Pi }({\mu }_{{{\rm{L}}}}{u}_{\Pi }+{\mu }_{{{\rm{T}}}}{R}_{\Pi }{\hat{h}}_{\Pi })\) . The parameters ( \({\alpha }_{{\rm{{L}}}}\) , \({\alpha }_{{{\rm{T}}}}\) ) and ( \({\mu }_{{\rm{{L}}}}\) , \({\mu }_{{{\rm{T}}}}\) ) are sets of laminar/turbulent parameters controlling air entrainment and drag resistance. These parameters, along with the turbulent decay parameter \({\beta }_{\Pi }\) control the magnitude of the avalanche air blast.
The vertical profiles of the velocity, density, and dynamic pressure, which are greatly influential to assess the air blast hazard, refer to Zhuang et al. 15 . The velocity profile follows a parabolic form and is determined using the boundary turbulent velocity values and the mean value. The density profile follows a linear profile decreasing from the bottom to the top of the cloud. Therefore, the vertical profile of the total pressure is written as \(P\left(z\right)=\frac{1}{2}\cdot {\rho }_{\Pi }\left(z\right)\cdot {{u}_{\Pi }\left(z\right)}^{2}=\frac{1}{2}\cdot {\rho }_{\Pi }\left(z\right)\cdot {[{\bar{u}}_{\Pi }(z)+{u{\prime} }_{\Pi }\left(z\right)]}^{2}\) . Here, we assume the worst case is that the fluctuation velocity is always in the same direction as the laminar mean velocity. In this study, we applied DEM arising from SPOT satellite images to do the simulation, referring to Ragettli et al. 44 .
The assessment of air blast-induced tree breakage follows the method proposed by Feistl et al. 27 . The tree bending stress arising from the air blast loading is
where \({c}_{\Pi }\) is the drag coefficient, \({\widetilde{u}}_{\Pi }\) is the instantaneous air blast velocity, which is the sum of the mean velocity \({\vec{u}}_{\Pi }\) and turbulent velocity \(u{\prime}\) , \({\rho }_{\Pi }\) is the cloud density, ( \(w\) , \(H\) , \(d\) ) represents the stem diameter, height and effective crown width of trees, respectively, \(\gamma\) is slope angle. The tree breakage occurs when the bending stress \({\sigma }_{\Pi }\) exceeds the experienced tree strength.
The dataset of air temperature used in this study is available at: https://doi.org/10.6084/m9.figshare.26178256 .
The RAMMS::RockIce model used in this study is available at https://ramms.ch/ .
Huggel, C., Caplan-Auerbach, J., Waythomas, C. F. & Wessels, R. L. Monitoring and modeling ice-rock avalanches from ice-capped volcanoes: a case study of frequent large avalanches on Iliamna Volcano, Alaska. J. Volcanol. Geotherm. Res. 168 , 114–136 (2007).
Article CAS Google Scholar
Schneider, D. et al. Insights into rock‐ice avalanche dynamics by combined analysis of seismic recordings and a numerical avalanche model. J. Geophys. Res.: Earth Surf. 115 , F04026 (2010).
Google Scholar
Shugar, D. H. et al. A massive rock and ice avalanche caused the 2021 disaster at Chamoli, Indian Himalaya. Science 373 , 300–306 (2021).
Gruber, S. et al. Review article: Inferring permafrost and permafrost thaw in the mountains of the Hindu Kush Himalaya region. Cryosphere 11 , 81–99 (2017).
Article Google Scholar
Ballesteros-Cánovas, J. A., Trappmann, D., Madrigal-González, J., Eckert, N. & Stoffel, M. Climate warming enhances snow avalanche risk in the Western Himalayas. Proc. Natl Acad. Sci. USA 115 , 3410–3415 (2018).
Kääb, A. et al. Massive collapse of two glaciers in western Tibet in 2016 after surge-like instability. Nat. Geosci. 11 , 114–120 (2018).
Fan, X. M. et al. Imminent threat of rock-ice avalanches in High Mountain Asia. Sci. Total Environ. 836 , 155380 (2022).
Bai, L. et al. Change in the spatiotemporal pattern of snowfall during the cold season under climate change in a snow-dominated region of China. Int. J. Climatol. 39 , 5702–2719 (2019).
Lin, W. & Chen, H. Changes in the spatial–temporal characteristics of daily snowfall events over the Eurasian continent from 1980 to 2019. Int. J. Climatol. 42 , 1841–1853 (2022).
Marshall, A. M., Link, T. E., Robinson, A. P. & Abatzoglou, J. T. Higher snowfall intensity is associated with reduced impacts of warming upon winter snow ablation. Geophys. Res. Lett. 47 , e2019GL086409 (2020).
Sovilla, B., Burlando, P. & Bartelt, P. Field experiments and numerical modeling of mass entrainment in snow avalanches. J. Geophys. Res.: Earth Surf. 111 , F03007 (2006).
Vera Valero, C., Wikstroemjones, K., Bühler, Y. & Bartelt, P. Release temperature, snow-cover entrainment and the thermal flow regime of snow avalanches. J. Glaciol. 61 , 173–184 (2015).
Vera Valero, C., Wever, N., Christen, M. & Bartelt, P. Modeling the influence of snow cover temperature and water content on wet-snow avalanche runout. Nat. Hazards Earth Syst. Sci. 18 , 869–887 (2018).
Bartelt, P., Buser, O., Vera Valero, C. & Bühler, Y. Configurational energy and the formation of mixed flowing powder snow and ice avalanches. Ann. Glaciol. 57 , 179–188 (2016).
Zhuang, Y. et al. Tree blow-down by snow avalanche air blasts: dynamic magnification effects and turbulence. Geophys. Res. Lett. 50 , e2023GL105334 (2023).
Vinnikov, K. Y. & Grody, N. C. Global warming trend of mean tropospheric temperature observed by satellites. Science 302 , 269–272 (2003).
Hansen, J. et al. Global temperature change. Proc. Natl Acad. Sci. USA 103 , 14288–14293 (2006).
Pudasaini, S. P. & Krautblatter, M. A two-phase mechanical model for rock-ice avalanches. J. Geophys. Res.: Earth Surf. 119 , 2272–2290 (2014).
Bartelt, P., Christen, M., Bühler, Y. & Buser, O. Thermomechanical modelling of rock avalanches with debris, ice and snow entrainment. Numer. Methods Geotech. Eng. IX. 2 , 1047–1054 (2018).
Pudasaini, S. P., & Hutter, K. Avalanche Dynamics: Dynamics of Rapid Flows of Dense Granular Avalanches (Springer-Verlag, Berlin, 2007).
Kisuka, F., Hare, C. & Wu, C. Y. Heat generation during oblique particle impact. Powder Technol. 422 , 118481 (2023).
Kargel, J. S. et al. Geomorphic and geologic controls of geohazards induced by Nepal’s 2015 Gorkha earthquake. Science 351 , aac8353 (2016).
Fujita, K. et al. Anomalous winter-snow-amplified earthquake-induced disaster of the 2015 Langtang avalanche in Nepal. Nat. Hazards Earth Syst. Sci. 17 , 749–764 (2017).
Zhuang, Y., Xu, Q., Xing, A., Bilal, M. & Gnyawali, K. R. Catastrophic air blasts triggered by large ice/rock avalanches. Landslides 20 , 53–64 (2023).
Lacroix, P. Landslides triggered by the Gorkha earthquake in the Langtang valley, volumes and initiation processes. Earth Planets Space 68 , 1–10 (2016).
Steiner, J. F. et al. Multi-year observations of the high mountain water cycle in the Langtang catchment, Central Himalaya. Hydrol. Process. 35 , e14189 (2021).
Feistl, T. et al. Forest damage and snow avalanche flow regime. Nat. Hazards Earth Syst. Sci. 15 , 1275–1288 (2015).
Yang, Q., Su, Z., Cheng, Q., Ren, Y. & Cai, F. High mobility of rock-ice avalanches: insights from small flume tests of gravel–ice mixtures. Eng. Geol. 260 , 105260 (2019).
Föhn, P. M. B., Camponovo, C. & Krüsi, G. Mechanical and structural properties of weak snow layers measured in situ. Ann. Glaciol. 26 , 1–6 (1998).
Bartelt, P., Buser, O. & Platzer, K. Starving avalanches: frictional mechanisms at the tails of finite-sized mass movements. Geophys. Res. Lett. 34 , L20407 (2007).
Sansone, S., Zugliani, D. & Rosatti, G. A mathematical framework for modelling rock-ice avalanches. J. Fluid Mech. 919 , A8 (2021).
Dong, Z. B. & Su, L. J. Flow regimes and basal normal stresses in rock–ice avalanches by experimental rotating drum tests. Cold Reg. Sci. Technol. 218 , 104081 (2024).
Ranz, W. & Marshall, W. Evaporation from drops. Chem. Eng. Prog. 48 , 141–146 (1952).
CAS Google Scholar
Bartelt, P. & McArdell, B. W. Granulometric investigations of snow avalanches. J. Glaciol. 55 , 829–833 (2009).
Gnyawali, K. R., Xing, A. G. & Zhuang, Y. Dynamic analysis of the multistaged ice-rock debris avalanche in the Langtang valley triggered by the 2015 Gorkha earthquake, Nepal. Eng. Geol. 265 , 105440 (2020).
Christen, M., Kowalski, J. & Bartelt, P. Numerical simulation of dense snow avalanches in three-dimensional terrain. Cold Reg. Sci. Technol. 63 , 1–14 (2010).
Frank, F. et al. Debris-flow modeling at Meretschibach and Bondasca catchments, Switzerland: sensitivity testing of field-data-based entrainment model. Nat. Hazards Earth Syst. Sci. 17 , 801–815 (2017).
Buser, O. & Bartelt, P. Production and decay of random kinetic energy in granular snow avalanches. J. Glaciol. 55 , 3–12 (2009).
Munch, J., Bartelt, P. & Christen, M. Multi-component avalanches for rock-and ice-falls to potential debris flow transition modelling. E3S Web Conf. 415 , 01017 (2023).
Salm, B. Flow, flow transition and runout distances of flowing avalanche. Ann. Glaciol. 18 , 221–226 (1993).
Richard, G. L. & Gavrilyuk, S. L. A new model of roll waves: comparison with Brock’s experiments. J. Fluid Mech. 698 , 374–405 (2012).
Vallet, J., Turnbull, B., Joly, S. & Dufour, F. Observations on powder snow avalanches using videogrammetry. Cold Reg. Sci. Technol. 39 , 153–159 (2004).
Turnbull, B. & McElwaine, J. N. A comparison of powder-snow avalanches at Valle´e de la Sionne, Switzerland, with plume theories. J. Glaciol. 53 , 30–40 (2007).
Ragettli, S., Bolch, T. & Pellicciotti, F. Heterogeneous glacier thinning patterns over the last 40 years in Langtang Himal, Nepal. Cryosphere 10 , 2075–2097 (2016).
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The authors are grateful to the late D.F. Breashears from GlacierWorks for the imagery taken from the helicopter, allowing us to identify the release areas of where the glaciers detached. This work is funded by the RAMMS project.
Authors and affiliations.
WSL Institute for Snow and Avalanche Research SLF, Davos Dorf, Switzerland
Yu Zhuang, Yves Bühler, Jessica Munch & Perry Bartelt
Climate Change, Extremes and Natural Hazards in Alpine Regions Research Centre CERC, Davos Dorf, Switzerland
Central Department of Hydrology and Meteorology, Tribhuvan University, Kathmandu, Nepal
Binod Dawadi
Kathmandu Center for Research and Education, Chinese Academy of Sciences-Tribhuvan University, Kathmandu, Nepal
Himalayan University Consortium, Lalitpur, Nepal
Jakob Steiner
Institute of Geography and Regional Science, University of Graz, Graz, Austria
Geotechnical Engineering and Geohazards (GEGH) Group, CSIR-Central Building Research Institute, Roorkee, Uttarakhand, India
Rajesh Kumar Dash
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Yu Zhuang designed the work, built the model, did the simulation, analyzed the results, and wrote the manuscript. Binod Dawadi, Rajesh Dash, and Yves Bühler did the field investigation and helped analyze the results. Jakob Steiner contributed to the paper revision and provided the release volume estimates, air temperature information, and DEM. Yves Bühler did an image analysis of the Langtang avalanche and created the satellite images. Jessica Munch helped with the numerical simulation. Perry Bartelt conceived the ideas, built the model, did the simulation, wrote and edited the manuscript.
Correspondence to Yu Zhuang .
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The authors declare no competing interests.
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Zhuang, Y., Dawadi, B., Steiner, J. et al. An earthquake-triggered avalanche in Nepal in 2015 was exacerbated by climate variability and snowfall anomalies. Commun Earth Environ 5 , 465 (2024). https://doi.org/10.1038/s43247-024-01624-z
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DOI : https://doi.org/10.1038/s43247-024-01624-z
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