Articles | Volume 10, issue 4
The Cryosphere, 10, 1721–1737, 2016
https://doi.org/10.5194/tc-10-1721-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The Cryosphere, 10, 1721–1737, 2016
https://doi.org/10.5194/tc-10-1721-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
11 Aug 2016
Research article
| 11 Aug 2016
Evaluation of air–soil temperature relationships simulated by land surface models during winter across the permafrost region
Wenli Wang et al.
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Cited
24 citations as recorded by crossref.
- Applicability of the ecosystem type approach to model permafrost dynamics across the Alaska North Slope D. Nicolsky et al. 10.1002/2016JF003852
- Model simulations of arctic biogeochemistry and permafrost extent are highly sensitive to the implemented snow scheme in LPJ-GUESS A. Pongracz et al. 10.5194/bg-18-5767-2021
- Mitigation of Arctic permafrost carbon loss through stratospheric aerosol geoengineering Y. Chen et al. 10.1038/s41467-020-16357-8
- Does tall vegetation warm or cool the ground surface? Constraining the ground thermal impacts of upright vegetation in northern environments R. Way & C. Lapalme 10.1088/1748-9326/abef31
- Effects of multilayer snow scheme on the simulation of snow: Offline Noah and coupled with NCEPCFSv2 S. Saha et al. 10.1002/2016MS000845
- ORCHIDEE-MICT (v8.4.1), a land surface model for the high latitudes: model description and validation M. Guimberteau et al. 10.5194/gmd-11-121-2018
- Effects of organic soil in the Noah-MP land-surface model on simulated skin and soil temperature profiles and surface energy exchanges for China G. Zhang et al. 10.1016/j.atmosres.2020.105284
- 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
- Uncertainties in coupled regional Arctic climate simulations associated with the used land surface model H. Matthes et al. 10.1002/2016JD026213
- Recent Changes in the ISBA‐CTRIP Land Surface System for Use in the CNRM‐CM6 Climate Model and in Global Off‐Line Hydrological Applications B. Decharme et al. 10.1029/2018MS001545
- Snow-Covered Soil Temperature Retrieval in Canadian Arctic Permafrost Areas, Using a Land Surface Scheme Informed with Satellite Remote Sensing Data N. Marchand et al. 10.3390/rs10111703
- Changes in the Response of the Northern Hemisphere Carbon Uptake to Temperature Over the Last Three Decades Y. Yin et al. 10.1029/2018GL077316
- Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change A. McGuire et al. 10.1073/pnas.1719903115
- Effects of short-term variability of meteorological variables on soil temperature in permafrost regions C. Beer et al. 10.5194/tc-12-741-2018
- Model-data fusion to assess year-round CO2 fluxes for an arctic heath ecosystem in West Greenland (69°N) W. Zhang et al. 10.1016/j.agrformet.2019.02.021
- New methods for calculating bare soil land surface temperature over mountainous terrain Y. Yang et al. 10.1007/s11629-016-4306-7
- Permafrost variability over the Northern Hemisphere based on the MERRA-2 reanalysis J. Tao et al. 10.5194/tc-13-2087-2019
- Soil moisture and hydrology projections of the permafrost region – a model intercomparison C. Andresen et al. 10.5194/tc-14-445-2020
- An ecological barrier between the Himalayas and the Hengduan Mountains maintains the disjunct distribution of Roscoea D. Li et al. 10.1111/jbi.13729
- Response of abiotic soil CO2 flux to the difference in air-soil temperature in a desert Y. Gao et al. 10.1016/j.scitotenv.2021.147377
- Vegetation can strongly regulate permafrost degradation at its southern edge through changing surface freeze-thaw processes W. Guo et al. 10.1016/j.agrformet.2018.01.010
- Impacts of snow on soil temperature observed across the circumpolar north Y. Zhang et al. 10.1088/1748-9326/aab1e7
- Characterizing Surface Albedo of Shallow Fresh Snow and Its Importance for Snow Ablation on the Interior of the Tibetan Plateau W. Wang et al. 10.1175/JHM-D-19-0193.1
- Observed Decrease in Soil and Atmosphere Temperature Coupling in Recent Decades Over Northern Eurasia L. Chen et al. 10.1029/2021GL092500
24 citations as recorded by crossref.
- Applicability of the ecosystem type approach to model permafrost dynamics across the Alaska North Slope D. Nicolsky et al. 10.1002/2016JF003852
- Model simulations of arctic biogeochemistry and permafrost extent are highly sensitive to the implemented snow scheme in LPJ-GUESS A. Pongracz et al. 10.5194/bg-18-5767-2021
- Mitigation of Arctic permafrost carbon loss through stratospheric aerosol geoengineering Y. Chen et al. 10.1038/s41467-020-16357-8
- Does tall vegetation warm or cool the ground surface? Constraining the ground thermal impacts of upright vegetation in northern environments R. Way & C. Lapalme 10.1088/1748-9326/abef31
- Effects of multilayer snow scheme on the simulation of snow: Offline Noah and coupled with NCEPCFSv2 S. Saha et al. 10.1002/2016MS000845
- ORCHIDEE-MICT (v8.4.1), a land surface model for the high latitudes: model description and validation M. Guimberteau et al. 10.5194/gmd-11-121-2018
- Effects of organic soil in the Noah-MP land-surface model on simulated skin and soil temperature profiles and surface energy exchanges for China G. Zhang et al. 10.1016/j.atmosres.2020.105284
- 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
- Uncertainties in coupled regional Arctic climate simulations associated with the used land surface model H. Matthes et al. 10.1002/2016JD026213
- Recent Changes in the ISBA‐CTRIP Land Surface System for Use in the CNRM‐CM6 Climate Model and in Global Off‐Line Hydrological Applications B. Decharme et al. 10.1029/2018MS001545
- Snow-Covered Soil Temperature Retrieval in Canadian Arctic Permafrost Areas, Using a Land Surface Scheme Informed with Satellite Remote Sensing Data N. Marchand et al. 10.3390/rs10111703
- Changes in the Response of the Northern Hemisphere Carbon Uptake to Temperature Over the Last Three Decades Y. Yin et al. 10.1029/2018GL077316
- Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change A. McGuire et al. 10.1073/pnas.1719903115
- Effects of short-term variability of meteorological variables on soil temperature in permafrost regions C. Beer et al. 10.5194/tc-12-741-2018
- Model-data fusion to assess year-round CO2 fluxes for an arctic heath ecosystem in West Greenland (69°N) W. Zhang et al. 10.1016/j.agrformet.2019.02.021
- New methods for calculating bare soil land surface temperature over mountainous terrain Y. Yang et al. 10.1007/s11629-016-4306-7
- Permafrost variability over the Northern Hemisphere based on the MERRA-2 reanalysis J. Tao et al. 10.5194/tc-13-2087-2019
- Soil moisture and hydrology projections of the permafrost region – a model intercomparison C. Andresen et al. 10.5194/tc-14-445-2020
- An ecological barrier between the Himalayas and the Hengduan Mountains maintains the disjunct distribution of Roscoea D. Li et al. 10.1111/jbi.13729
- Response of abiotic soil CO2 flux to the difference in air-soil temperature in a desert Y. Gao et al. 10.1016/j.scitotenv.2021.147377
- Vegetation can strongly regulate permafrost degradation at its southern edge through changing surface freeze-thaw processes W. Guo et al. 10.1016/j.agrformet.2018.01.010
- Impacts of snow on soil temperature observed across the circumpolar north Y. Zhang et al. 10.1088/1748-9326/aab1e7
- Characterizing Surface Albedo of Shallow Fresh Snow and Its Importance for Snow Ablation on the Interior of the Tibetan Plateau W. Wang et al. 10.1175/JHM-D-19-0193.1
- Observed Decrease in Soil and Atmosphere Temperature Coupling in Recent Decades Over Northern Eurasia L. Chen et al. 10.1029/2021GL092500
Latest update: 03 Jul 2022
Short summary
The winter snow insulation is a key process for air–soil temperature coupling and is relevant for permafrost simulations. Differences in simulated air–soil temperature relationships and their modulation by climate conditions are found to be related to the snow model physics. Generally, models with better performance apply multilayer snow schemes.
The winter snow insulation is a key process for air–soil temperature coupling and is relevant...
