Articles | Volume 17, issue 3
https://doi.org/10.5194/cp-17-1161-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-1161-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The role of land cover in the climate of glacial Europe
Patricio Velasquez
CORRESPONDING AUTHOR
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
Jed O. Kaplan
Department of Earth Sciences, The University of Hong Kong, Hong Kong SAR, China
Martina Messmer
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
School of Earth Sciences, The University of Melbourne, Melbourne, Victoria, Australia
Patrick Ludwig
Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
Christoph C. Raible
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
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Cited
15 citations as recorded by crossref.
- Subalpine tall-herb vegetation in Bulgaria: diversity and ecology D. Szokala et al. 10.1080/11263504.2024.2327865
- Opening up the peer review process N. Hynninen 10.1075/jerpp.21025.hyn
- Simulations of the Holocene climate in Europe using an interactive downscaling within the iLOVECLIM model (version 1.1) F. Arthur et al. 10.5194/cp-19-87-2023
- Atmosphere–cryosphere interactions during the last phase of the Last Glacial Maximum (21 ka) in the European Alps C. Del Gobbo et al. 10.5194/cp-19-1805-2023
- Insights into the Australian mid-Holocene climate using downscaled climate models A. Lowry & H. McGowan 10.5194/cp-20-2309-2024
- Mid-Holocene European climate revisited: New high-resolution regional climate model simulations using pollen-based land-cover G. Strandberg et al. 10.1016/j.quascirev.2022.107431
- Coupled climate-glacier modelling of the last glaciation in the Alps G. Jouvet et al. 10.1017/jog.2023.74
- The climate and vegetation of Europe, northern Africa, and the Middle East during the Last Glacial Maximum (21 000 yr BP) based on pollen data B. Davis et al. 10.5194/cp-20-1939-2024
- Is there a massive glacial–Holocene flora continuity in Central Europe? Á. Molnár et al. 10.1111/brv.13007
- Did the Bronze Age deforestation of Europe affect its climate? A regional climate model study using pollen-based land cover reconstructions G. Strandberg et al. 10.5194/cp-19-1507-2023
- The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
- Speleothem growth and stable carbon isotopes as proxies of the presence and thermodynamical state of glaciers compared to modelled glacier evolution in the Alps V. Skiba et al. 10.1016/j.quascirev.2023.108403
- Verification of paleo reconstructions of climatic conditions of the Late Pleistocene summer seasons based on palynological analysis of Yedoma deposits and ice wedges A. Vasil'chuk & Y. Vasil'chuk 10.7256/2453-8922.2021.4.36787
- High-resolution LGM climate of Europe and the Alpine region using the regional climate model WRF E. Russo et al. 10.5194/cp-20-449-2024
- Last Glacial Maximum glacier fluctuations on the northern Alpine foreland: Geomorphological and chronological reconstructions from the Rhine and Reuss glacier systems S. Kamleitner et al. 10.1016/j.geomorph.2022.108548
15 citations as recorded by crossref.
- Subalpine tall-herb vegetation in Bulgaria: diversity and ecology D. Szokala et al. 10.1080/11263504.2024.2327865
- Opening up the peer review process N. Hynninen 10.1075/jerpp.21025.hyn
- Simulations of the Holocene climate in Europe using an interactive downscaling within the iLOVECLIM model (version 1.1) F. Arthur et al. 10.5194/cp-19-87-2023
- Atmosphere–cryosphere interactions during the last phase of the Last Glacial Maximum (21 ka) in the European Alps C. Del Gobbo et al. 10.5194/cp-19-1805-2023
- Insights into the Australian mid-Holocene climate using downscaled climate models A. Lowry & H. McGowan 10.5194/cp-20-2309-2024
- Mid-Holocene European climate revisited: New high-resolution regional climate model simulations using pollen-based land-cover G. Strandberg et al. 10.1016/j.quascirev.2022.107431
- Coupled climate-glacier modelling of the last glaciation in the Alps G. Jouvet et al. 10.1017/jog.2023.74
- The climate and vegetation of Europe, northern Africa, and the Middle East during the Last Glacial Maximum (21 000 yr BP) based on pollen data B. Davis et al. 10.5194/cp-20-1939-2024
- Is there a massive glacial–Holocene flora continuity in Central Europe? Á. Molnár et al. 10.1111/brv.13007
- Did the Bronze Age deforestation of Europe affect its climate? A regional climate model study using pollen-based land cover reconstructions G. Strandberg et al. 10.5194/cp-19-1507-2023
- The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
- Speleothem growth and stable carbon isotopes as proxies of the presence and thermodynamical state of glaciers compared to modelled glacier evolution in the Alps V. Skiba et al. 10.1016/j.quascirev.2023.108403
- Verification of paleo reconstructions of climatic conditions of the Late Pleistocene summer seasons based on palynological analysis of Yedoma deposits and ice wedges A. Vasil'chuk & Y. Vasil'chuk 10.7256/2453-8922.2021.4.36787
- High-resolution LGM climate of Europe and the Alpine region using the regional climate model WRF E. Russo et al. 10.5194/cp-20-449-2024
- Last Glacial Maximum glacier fluctuations on the northern Alpine foreland: Geomorphological and chronological reconstructions from the Rhine and Reuss glacier systems S. Kamleitner et al. 10.1016/j.geomorph.2022.108548
Latest update: 14 Nov 2024
Short summary
This study assesses the importance of resolution and land–atmosphere feedbacks for European climate. We performed an asynchronously coupled experiment that combined a global climate model (~ 100 km), a regional climate model (18 km), and a dynamic vegetation model (18 km). Modelled climate and land cover agree reasonably well with independent reconstructions based on pollen and other paleoenvironmental proxies. The regional climate is significantly influenced by land cover.
This study assesses the importance of resolution and land–atmosphere feedbacks for European...