Articles | Volume 13, issue 3
https://doi.org/10.5194/gmd-13-1663-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-13-1663-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Lower boundary conditions in land surface models – effects on the permafrost and the carbon pools: a case study with CLM4.5
Ignacio Hermoso de Mendoza
Centre de Recherche sur la dynamique du système Terre (GEOTOP), Université du Québec à Montréal (UQAM), Montréal, Québec, Canada
Climate & Atmospheric Sciences Institute and Department of Earth Sciences, St. Francis Xavier University, Antigonish, Nova Scotia, Canada
Andrew H. MacDougall
Climate & Atmospheric Sciences Institute and Department of Earth Sciences, St. Francis Xavier University, Antigonish, Nova Scotia, Canada
Jean-Claude Mareschal
Centre de Recherche sur la dynamique du système Terre (GEOTOP), Université du Québec à Montréal (UQAM), Montréal, Québec, Canada
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Cited
21 citations as recorded by crossref.
- First assessment of the earth heat inventory within CMIP5 historical simulations F. Cuesta-Valero et al. 10.5194/esd-12-581-2021
- Heat stored in the Earth system: where does the energy go? K. von Schuckmann et al. 10.5194/essd-12-2013-2020
- Evaluating permafrost definitions for global permafrost area estimates in CMIP6 climate models N. Steinert et al. 10.1088/1748-9326/ad10d7
- A new bootstrap technique to quantify uncertainty in estimates of ground surface temperature and ground heat flux histories from geothermal data F. Cuesta-Valero et al. 10.5194/gmd-15-7913-2022
- Evaluation of the Performance of CLM5.0 in Soil Hydrothermal Dynamics in Permafrost Regions on the Qinghai–Tibet Plateau S. Yang et al. 10.3390/rs14246228
- Investigating the thermal state of permafrost with Bayesian inverse modeling of heat transfer B. Groenke et al. 10.5194/tc-17-3505-2023
- Evaluation of Parameterization Schemes for Matric Potential in Frozen Soil in Land Surface Models: A Modeling Perspective Y. Zhao et al. 10.1029/2023WR034644
- First comprehensive assessment of industrial-era land heat uptake from multiple sources F. García-Pereira et al. 10.5194/esd-15-547-2024
- Continental heat storage: contributions from the ground, inland waters, and permafrost thawing F. Cuesta-Valero et al. 10.5194/esd-14-609-2023
- Quantification and practical solution for bottom boundary effects on long-term permafrost models C. Ross et al. 10.1139/cgj-2023-0627
- First Quantification of the Permafrost Heat Sink in the Earth's Climate System J. Nitzbon et al. 10.1029/2022GL102053
- Hydrologic‐land surface modelling of the Canadian sporadic‐discontinuous permafrost: Initialization and uncertainty propagation M. Abdelhamed et al. 10.1002/hyp.14509
- Effects of a long‐term anoxic warming scenario on microbial community structure and functional potential of permafrost‐affected soil S. Yang et al. 10.1002/ppp.2131
- Increasing the Depth of a Land Surface Model. Part I: Impacts on the Subsurface Thermal Regime and Energy Storage J. González-Rouco et al. 10.1175/JHM-D-21-0024.1
- Assessment of a hydrologic-land surface model to simulate thermo-hydrologic evolution of permafrost regions M. Abdelhamed et al. 10.1016/j.jhydrol.2024.132161
- Increasing the Depth of a Land Surface Model. Part II: Temperature Sensitivity to Improved Subsurface Thermodynamics and Associated Permafrost Response N. Steinert et al. 10.1175/JHM-D-21-0023.1
- Challenges in Hydrologic‐Land Surface Modeling of Permafrost Signatures—A Canadian Perspective M. Abdelhamed et al. 10.1029/2022MS003013
- The evolution of Arctic permafrost over the last 3 centuries from ensemble simulations with the CryoGridLite permafrost model M. Langer et al. 10.5194/tc-18-363-2024
- Thermodynamic and hydrological drivers of the soil and bedrock thermal regimes in central Spain F. García-Pereira et al. 10.5194/soil-10-1-2024
- Agreement of Analytical and Simulation‐Based Estimates of the Required Land Depth in Climate Models N. Steinert et al. 10.1029/2021GL094273
- Impacts of seasonally frozen soil hydrothermal dynamics on the watershed hydrological processes inferred from a spatially distributed numerical modelling approach H. Gao et al. 10.1016/j.jhydrol.2023.129947
21 citations as recorded by crossref.
- First assessment of the earth heat inventory within CMIP5 historical simulations F. Cuesta-Valero et al. 10.5194/esd-12-581-2021
- Heat stored in the Earth system: where does the energy go? K. von Schuckmann et al. 10.5194/essd-12-2013-2020
- Evaluating permafrost definitions for global permafrost area estimates in CMIP6 climate models N. Steinert et al. 10.1088/1748-9326/ad10d7
- A new bootstrap technique to quantify uncertainty in estimates of ground surface temperature and ground heat flux histories from geothermal data F. Cuesta-Valero et al. 10.5194/gmd-15-7913-2022
- Evaluation of the Performance of CLM5.0 in Soil Hydrothermal Dynamics in Permafrost Regions on the Qinghai–Tibet Plateau S. Yang et al. 10.3390/rs14246228
- Investigating the thermal state of permafrost with Bayesian inverse modeling of heat transfer B. Groenke et al. 10.5194/tc-17-3505-2023
- Evaluation of Parameterization Schemes for Matric Potential in Frozen Soil in Land Surface Models: A Modeling Perspective Y. Zhao et al. 10.1029/2023WR034644
- First comprehensive assessment of industrial-era land heat uptake from multiple sources F. García-Pereira et al. 10.5194/esd-15-547-2024
- Continental heat storage: contributions from the ground, inland waters, and permafrost thawing F. Cuesta-Valero et al. 10.5194/esd-14-609-2023
- Quantification and practical solution for bottom boundary effects on long-term permafrost models C. Ross et al. 10.1139/cgj-2023-0627
- First Quantification of the Permafrost Heat Sink in the Earth's Climate System J. Nitzbon et al. 10.1029/2022GL102053
- Hydrologic‐land surface modelling of the Canadian sporadic‐discontinuous permafrost: Initialization and uncertainty propagation M. Abdelhamed et al. 10.1002/hyp.14509
- Effects of a long‐term anoxic warming scenario on microbial community structure and functional potential of permafrost‐affected soil S. Yang et al. 10.1002/ppp.2131
- Increasing the Depth of a Land Surface Model. Part I: Impacts on the Subsurface Thermal Regime and Energy Storage J. González-Rouco et al. 10.1175/JHM-D-21-0024.1
- Assessment of a hydrologic-land surface model to simulate thermo-hydrologic evolution of permafrost regions M. Abdelhamed et al. 10.1016/j.jhydrol.2024.132161
- Increasing the Depth of a Land Surface Model. Part II: Temperature Sensitivity to Improved Subsurface Thermodynamics and Associated Permafrost Response N. Steinert et al. 10.1175/JHM-D-21-0023.1
- Challenges in Hydrologic‐Land Surface Modeling of Permafrost Signatures—A Canadian Perspective M. Abdelhamed et al. 10.1029/2022MS003013
- The evolution of Arctic permafrost over the last 3 centuries from ensemble simulations with the CryoGridLite permafrost model M. Langer et al. 10.5194/tc-18-363-2024
- Thermodynamic and hydrological drivers of the soil and bedrock thermal regimes in central Spain F. García-Pereira et al. 10.5194/soil-10-1-2024
- Agreement of Analytical and Simulation‐Based Estimates of the Required Land Depth in Climate Models N. Steinert et al. 10.1029/2021GL094273
- Impacts of seasonally frozen soil hydrothermal dynamics on the watershed hydrological processes inferred from a spatially distributed numerical modelling approach H. Gao et al. 10.1016/j.jhydrol.2023.129947
Latest update: 17 Nov 2024
Short summary
We study the impact that the thickness of the subsurface and the geothermal gradient have in land models for climate simulations. To do this, we modify the Community Land Model version 4.5. In a scenario of rising atmospheric temperatures, the temperature of an insufficiently deep subsurface rises faster than it would in the real land. For the model, this produces faster permafrost thawing and increased emissions of land carbon to the atmosphere.
We study the impact that the thickness of the subsurface and the geothermal gradient have in...