38 citations as recorded by crossref.

1. How do forest fires affect soil greenhouse gas emissions in upland boreal forests? A review C. Ribeiro-Kumara et al. 10.1016/j.envres.2020.109328
2. Machine learning-based thermokarst landslide susceptibility modeling across the permafrost region on the Qinghai-Tibet Plateau G. Yin et al. 10.1007/s10346-021-01669-7
3. Significant shallow–depth soil warming over Russia during the past 40 years L. Chen et al. 10.1016/j.gloplacha.2020.103394
4. Effects of Climate Variability on Malaria Transmission in Southern Côte d’Ivoire, West Africa M. Doumbia et al. 10.3390/ijerph20237102
5. Thawing permafrost can mitigate warming-induced drought stress in boreal forest trees A. Kirdyanov et al. 10.1016/j.scitotenv.2023.168858
6. Contrasting characteristics, changes, and linkages of permafrost between the Arctic and the Third Pole X. Wang et al. 10.1016/j.earscirev.2022.104042
7. Daily station-level records of air temperature, snow depth, and ground temperature in the Northern Hemisphere V. Tran et al. 10.1038/s41597-024-03483-x
8. Effects of snow manipulation on larch trees in the taiga forest ecosystem in northeastern Siberia R. Shakhmatov et al. 10.1186/s40645-021-00460-5
9. The impacts of vegetation on the soil surface freezing-thawing processes at permafrost southern edge simulated by an improved process-based ecosystem model Z. Liu et al. 10.1016/j.ecolmodel.2021.109663
10. Spatial Analyses and Susceptibility Modeling of Thermokarst Lakes in Permafrost Landscapes along the Qinghai–Tibet Engineering Corridor G. Yin et al. 10.3390/rs13101974
11. Nordic boreo-arctic lands under rapid climatic change: A review of recent and future trends and extreme events J. Bjerke et al. 10.1016/j.earscirev.2024.105012
12. Observed Decrease in Soil and Atmosphere Temperature Coupling in Recent Decades Over Northern Eurasia L. Chen et al. 10.1029/2021GL092500
13. High potential for loss of permafrost landforms in a changing climate O. Karjalainen et al. 10.1088/1748-9326/abafd5
14. Divergent responses of permafrost degradation to precipitation increases at different seasons on the eastern Qinghai–Tibet Plateau based on modeling approach J. Yang et al. 10.1088/1748-9326/acf05c
15. Contrasting sensitivity of air temperature trends to surface soil temperature trends between climate models and reanalyses Y. Qiao et al. 10.1038/s41612-024-00588-3
16. Impact process and mechanism of summertime rainfall on thermal–moisture regime of active layer in permafrost regions of central Qinghai–Tibet Plateau M. Zhang et al. 10.1016/j.scitotenv.2021.148970
17. Limited sensitivity of permafrost soils to heavy rainfall across Svalbard ecosystems R. Magnússon et al. 10.1016/j.scitotenv.2024.173696
18. A novel framework for multiple thermokarst hazards risk assessment and controlling environmental factors analysis on the Qinghai-Tibet Plateau P. Lou et al. 10.1016/j.catena.2024.108367
19. Maximum summer temperatures predict the temperature adaptation of Arctic soil bacterial communities R. Rijkers et al. 10.5194/bg-20-767-2023
20. Impact of climate warming on permafrost changes in the Qinghai-Tibet Plateau R. Li et al. 10.1016/j.coldregions.2022.103692
21. Evaluating permafrost definitions for global permafrost area estimates in CMIP6 climate models N. Steinert et al. 10.1088/1748-9326/ad10d7
22. Surface energy balance of sub‐Arctic roads with varying snow regimes and properties in permafrost regions L. Chen et al. 10.1002/ppp.2129
23. Changes in permafrost spatial distribution and active layer thickness from 1980 to 2020 on the Tibet Plateau T. Shen et al. 10.1016/j.scitotenv.2022.160381
24. Permafrost thawing puts the frozen carbon at risk over the Tibetan Plateau T. Wang et al. 10.1126/sciadv.aaz3513
25. Evaluating permafrost physics in the Coupled Model Intercomparison Project 6 (CMIP6) models and their sensitivity to climate change E. Burke et al. 10.5194/tc-14-3155-2020
26. Thermal regime variations of the uppermost soil layer in the central Tibetan Plateau R. Chen et al. 10.1016/j.catena.2022.106224
27. Daily soil temperature simulation at different depths in the Red River Basin: a long short-term memory approach M. Tahmasebi Nasab et al. 10.1007/s40808-024-01988-3
28. The ERA5-Land soil temperature bias in permafrost regions B. Cao et al. 10.5194/tc-14-2581-2020
29. Effects of increasing rainfall on organic carbon release and transport processes in permafrost on the central Tibetan Plateau H. Wei et al. 10.1016/j.catena.2024.108553
30. Remote sensing spatiotemporal patterns of frozen soil and the environmental controls over the Tibetan Plateau during 2002–2016 G. Zheng et al. 10.1016/j.rse.2020.111927
31. Data-driven spatiotemporal projections of shallow permafrost based on CMIP6 across the Qinghai‒Tibet Plateau at 1 km2 scale G. Yin et al. 10.1016/j.accre.2021.08.009
32. Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale O. Leppiniemi et al. 10.5194/tc-17-3157-2023
33. Susceptibility Mapping of Thaw Slumps Based on Neural Network Methods along the Qinghai–Tibet Engineering Corridor P. Li et al. 10.3390/su16125120
34. Convective heat transfer of spring meltwater accelerates active layer phase change in Tibet permafrost areas Y. Zhao et al. 10.5194/tc-16-825-2022
35. What conditions favor the influence of seasonally frozen ground on hydrological partitioning? A systematic review P. Ala-Aho et al. 10.1088/1748-9326/abe82c
36. Thermokarst Lake Susceptibility Assessment Induced by Permafrost Degradation in the Qinghai–Tibet Plateau Using Machine Learning Methods R. Wang et al. 10.3390/rs15133331
37. Investigating the sensitivity of soil heterotrophic respiration to recent snow cover changes in Alaska using a satellite-based permafrost carbon model Y. Yi et al. 10.5194/bg-17-5861-2020
38. Continentality determines warming or cooling impact of heavy rainfall events on permafrost A. Hamm et al. 10.1038/s41467-023-39325-4