Articles | Volume 12, issue 1
https://doi.org/10.5194/cp-12-151-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-151-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
29 Jan 2016
Research article |
| 29 Jan 2016
The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum
M. Stärz
CORRESPONDING AUTHOR
Alfred Wegener Institute Helmholtz Centre for Polar and
Marine Research, Bremerhaven, Germany
Senckenberg Research Institute and Natural History Museum,
Frankfurt am Main, Germany
Biodiversity and Climate Research Centre (LOEWE BiK-F),
Frankfurt am Main, Germany
G. Lohmann
Alfred Wegener Institute Helmholtz Centre for Polar and
Marine Research, Bremerhaven, Germany
University of Bremen, Bremen, Germany
Alfred Wegener Institute Helmholtz Centre for Polar and
Marine Research, Bremerhaven, Germany
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Cited
14 citations as recorded by crossref.
- ESD Ideas: The stochastic climate model shows that underestimated Holocene trends and variability represent two sides of the same coin G. Lohmann https://doi.org/10.5194/esd-9-1279-2018
- On the mechanisms of warming the mid-Pliocene and the inference of a hierarchy of climate sensitivities with relevance to the understanding of climate futures D. Chandan & W. Peltier https://doi.org/10.5194/cp-14-825-2018
- A Modeling Perspective on the Lingering Glacial Sea Surface Temperature Conundrum S. Krätschmer et al. https://doi.org/10.1029/2022GL100378
- Impact of Weddell Sea shelf progradation on Antarctic bottom water formation during the Miocene X. Huang et al. https://doi.org/10.1002/2016PA002987
- Climate change shifts the distribution of vegetation types in South Brazilian hotspots W. Trindade et al. https://doi.org/10.1007/s10113-020-01686-7
- Speleothems of South American and Asian Monsoons Influenced by a Green Sahara C. Tabor et al. https://doi.org/10.1029/2020GL089695
- Summer temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20 000 years V. Meyer et al. https://doi.org/10.5194/cp-13-359-2017
- Mid-to-late Holocene temperature evolution and atmospheric dynamics over Europe in regional model simulations E. Russo & U. Cubasch https://doi.org/10.5194/cp-12-1645-2016
- Opening of the Fram Strait led to the establishment of a modern-like three-layer stratification in the Arctic Ocean during the Miocene A. Hossain et al. https://doi.org/10.1007/s41063-020-00079-8
- Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge M. Stärz et al. https://doi.org/10.1038/ncomms15681
- Greenland Ice Sheet influence on Last Interglacial climate: global sensitivity studies performed with an atmosphere–ocean general circulation model M. Pfeiffer & G. Lohmann https://doi.org/10.5194/cp-12-1313-2016
- Simulated Thermohaline Fingerprints in Response to Different Greenland‐Scotland Ridge and Fram Strait Subsidence Histories A. Hossain et al. https://doi.org/10.1029/2019PA003842
- Mid-Holocene climate over the Mediterranean, North Africa, and Middle East simulated using a regional climate model F. Xie et al. https://doi.org/10.1177/09596836251350243
- Contribution of the coupled atmosphere–ocean–sea ice–vegetation model COSMOS to the PlioMIP2 C. Stepanek et al. https://doi.org/10.5194/cp-16-2275-2020
14 citations as recorded by crossref.
- ESD Ideas: The stochastic climate model shows that underestimated Holocene trends and variability represent two sides of the same coin G. Lohmann https://doi.org/10.5194/esd-9-1279-2018
- On the mechanisms of warming the mid-Pliocene and the inference of a hierarchy of climate sensitivities with relevance to the understanding of climate futures D. Chandan & W. Peltier https://doi.org/10.5194/cp-14-825-2018
- A Modeling Perspective on the Lingering Glacial Sea Surface Temperature Conundrum S. Krätschmer et al. https://doi.org/10.1029/2022GL100378
- Impact of Weddell Sea shelf progradation on Antarctic bottom water formation during the Miocene X. Huang et al. https://doi.org/10.1002/2016PA002987
- Climate change shifts the distribution of vegetation types in South Brazilian hotspots W. Trindade et al. https://doi.org/10.1007/s10113-020-01686-7
- Speleothems of South American and Asian Monsoons Influenced by a Green Sahara C. Tabor et al. https://doi.org/10.1029/2020GL089695
- Summer temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20 000 years V. Meyer et al. https://doi.org/10.5194/cp-13-359-2017
- Mid-to-late Holocene temperature evolution and atmospheric dynamics over Europe in regional model simulations E. Russo & U. Cubasch https://doi.org/10.5194/cp-12-1645-2016
- Opening of the Fram Strait led to the establishment of a modern-like three-layer stratification in the Arctic Ocean during the Miocene A. Hossain et al. https://doi.org/10.1007/s41063-020-00079-8
- Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge M. Stärz et al. https://doi.org/10.1038/ncomms15681
- Greenland Ice Sheet influence on Last Interglacial climate: global sensitivity studies performed with an atmosphere–ocean general circulation model M. Pfeiffer & G. Lohmann https://doi.org/10.5194/cp-12-1313-2016
- Simulated Thermohaline Fingerprints in Response to Different Greenland‐Scotland Ridge and Fram Strait Subsidence Histories A. Hossain et al. https://doi.org/10.1029/2019PA003842
- Mid-Holocene climate over the Mediterranean, North Africa, and Middle East simulated using a regional climate model F. Xie et al. https://doi.org/10.1177/09596836251350243
- Contribution of the coupled atmosphere–ocean–sea ice–vegetation model COSMOS to the PlioMIP2 C. Stepanek et al. https://doi.org/10.5194/cp-16-2275-2020
Saved (final revised paper)
Latest update: 14 Jun 2026
Short summary
In order to account for coupled climate-soil processes, we developed a soil scheme which is asynchronously coupled to an earth system model. We tested the scheme and found additional warming for a relatively warm climate (mid-Holocene), and extra cooling for a colder (Last Glacial Maximum) than preindustrial climate. These findings indicate a relatively strong positive soil feedback to climate, which may help to reduce model-data discrepancies for the climate of the geological past.
In order to account for coupled climate-soil processes, we developed a soil scheme which is...
