39 citations as recorded by crossref.

1. Cascading effects of climate change and wildfire on a subarctic lake: A 20‐year case study of watershed change A. Larsen et al. 10.1002/ecs2.4558
2. Influence of Wildfire on Downstream Transport of Dissolved Carbon, Nutrients, and Mercury in the Permafrost Zone of Boreal Western Canada R. Hutchins et al. 10.1029/2023JG007602
3. Multi‐year high‐frequency sampling provides new runoff and biogeochemical insights in a discontinuous permafrost watershed N. Shatilla et al. 10.1002/hyp.14898
4. Enhanced home-field advantage in deep soil organic carbon decomposition: Insights from soil transplantation in subtropical forests K. Liang et al. 10.1016/j.scitotenv.2024.171596
5. Large stocks of peatland carbon and nitrogen are vulnerable to permafrost thaw G. Hugelius et al. 10.1073/pnas.1916387117
6. Assessing the Potential for Mobilization of Old Soil Carbon After Permafrost Thaw: A Synthesis of 14C Measurements From the Northern Permafrost Region C. Estop‐Aragonés et al. 10.1029/2020GB006672
7. Water pollution risks by smoldering fires in degraded peatlands H. Liu et al. 10.1016/j.scitotenv.2023.161979
8. Assessing inter-annual and seasonal patterns of DOC and DOM quality across a complex alpine watershed underlain by discontinuous permafrost in Yukon, Canada N. Shatilla & S. Carey 10.5194/hess-23-3571-2019
9. Variation in riverine dissolved organic matter (DOM) optical quality during snowmelt- and rainfall-driven events in a forested wetland watershed L. Rose et al. 10.1016/j.jhydrol.2022.128988
10. Thaw-induced impacts on land and water in discontinuous permafrost: A review of the Taiga Plains and Taiga Shield, northwestern Canada S. Wright et al. 10.1016/j.earscirev.2022.104104
11. Concentrations and Yields of Mercury, Methylmercury, and Dissolved Organic Carbon From Contrasting Catchments in the Discontinuous Permafrost Region, Western Canada L. Thompson et al. 10.1029/2023WR034848
12. Magnitude and drivers of integrated fluvial network greenhouse gas emissions across the boreal landscape in Québec R. Hutchins et al. 10.1016/j.watres.2020.115556
13. Wildfire impacts on surface water quality parameters: Cause of data variability and reporting needs O. Raoelison et al. 10.1016/j.envpol.2022.120713
14. Effect of fire on characteristics of dissolved organic matter in forested catchments in the Mediterranean biome: A review K. Tshering et al. 10.1016/j.watres.2022.119490
15. Permafrost thaw causes large carbon loss in boreal peatlands while changes to peat quality are limited L. Harris et al. 10.1111/gcb.16894
16. Impact of wildfire on permafrost landscapes: A review of recent advances and future prospects J. Holloway et al. 10.1002/ppp.2048
17. Modelling Watershed and River Basin Processes in Cold Climate Regions: A Review J. Wang et al. 10.3390/w13040518
18. Assessing leached TOC, nutrients and phenols from peatland soils after lab-simulated wildfires: Implications to source water protection Y. Wu et al. 10.1016/j.scitotenv.2022.153579
19. Effects of Prescribed Burn on Nutrient and Dissolved Organic Matter Characteristics in Peatland Shallow Groundwater J. Orlova et al. 10.3390/fire3030053
20. Opposing Effects of Climate and Permafrost Thaw on CH4 and CO2 Emissions From Northern Lakes M. Kuhn et al. 10.1029/2021AV000515
21. Aged soils contribute little to contemporary carbon cycling downstream of thawing permafrost peatlands A. Tanentzap et al. 10.1111/gcb.15756
22. Severe western Canadian wildfire affects water quality even at large basin scales C. Emmerton et al. 10.1016/j.watres.2020.116071
23. Isotope applications to soil science at the University of Alberta — an historical perspective B. Feland et al. 10.1139/cjss-2019-0153
24. Advances in wetland hydrology: the Canadian contribution over 75 years J. Price et al. 10.1080/07011784.2023.2269137
25. Improving hydrologic model to predict the effect of snowpack and soil temperature on carbon dioxide emission in the cold region peatlands N. Melaku et al. 10.1016/j.jhydrol.2020.124939
26. High ebullitive, millennial‐aged greenhouse gas emissions from thermokarst expansion of peatland lakes in boreal western Canada M. Kuhn et al. 10.1002/lno.12288
27. Assessing Leached Toc, Nutrients and Phenols from Peatland Soils after Lab-Simulated Wildfires: Implications to Source Water Protection Y. Wu et al. 10.2139/ssrn.3967440
28. Western Canadian freshwater availability: current and future vulnerabilities B. Bonsal et al. 10.1139/er-2020-0040
29. Hydrogeologic setting overrides any influence of wildfire on pore water dissolved organic carbon concentration and quality at a boreal fen S. Davidson et al. 10.1002/eco.2141
30. Plant Uptake Offsets Silica Release From a Large Arctic Tundra Wildfire J. Carey et al. 10.1029/2019EF001149
31. Impact factors of dissolved organic carbon and the transport in a river-lake continuum in the Tibet Plateau of China Z. Wen et al. 10.1016/j.jhydrol.2019.124202
32. Mid-term post-fire losses of nitrogen and phosphorus by overland flow in two contrasting eucalypt stands in north-central Portugal D. Serpa et al. 10.1016/j.scitotenv.2019.135843
33. Fluvial CO2 and CH4 patterns across wildfire‐disturbed ecozones of subarctic Canada: Current status and implications for future change R. Hutchins et al. 10.1111/gcb.14960
34. Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau X. You et al. 10.3390/su14042441
35. A synthesis of three decades of hydrological research at Scotty Creek, NWT, Canada W. Quinton et al. 10.5194/hess-23-2015-2019
36. Lability of dissolved organic carbon from boreal peatlands: interactions between permafrost thaw, wildfire, and season K. Burd et al. 10.1139/cjss-2019-0154
37. The impact of wildfire on biogeochemical fluxes and water quality in boreal catchments G. Granath et al. 10.5194/bg-18-3243-2021
38. Fire Characteristics and Hydrologic Connectivity Influence Short‐Term Responses of North Temperate Lakes to Wildfire I. McCullough et al. 10.1029/2023GL103953
39. Wildfires lead to decreased carbon and increased nitrogen concentrations in upland arctic streams B. Rodríguez-Cardona et al. 10.1038/s41598-020-65520-0