The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum

• Published in: Climate of the Past
• Main Authors: Stärz, M., Lohmann, G., Knorr, G.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2016
• Subjects: article; Verlagsveröffentlichung; taiga; Tundra
• Online Access: https://doi.org/10.5194/cp-12-151-2016; https://noa.gwlb.de/receive/cop_mods_00014161; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00014117/cp-12-151-2016.pdf; https://cp.copernicus.org/articles/12/151/2016/cp-12-151-2016.pdf

In order to account for coupled climate–soil processes, we have developed a soil scheme which is asynchronously coupled to a comprehensive climate model with dynamic vegetation. This scheme considers vegetation as the primary control of changes in physical soil characteristics. We test the scheme for a warmer (mid-Holocene) and colder (Last Glacial Maximum) climate relative to the preindustrial climate. We find that the computed changes in physical soil characteristics lead to significant amplification of global climate anomalies, representing a positive feedback. The inclusion of the soil feedback yields an extra surface warming of 0.24 °C for the mid-Holocene and an additional global cooling of 1.07 °C for the Last Glacial Maximum. Transition zones such as desert–savannah and taiga–tundra exhibit a pronounced response in the model version with dynamic soil properties. Energy balance model analyses reveal that our soil scheme amplifies the temperature anomalies in the mid-to-high northern latitudes via changes in the planetary albedo and the effective longwave emissivity. As a result of the modified soil treatment and the positive feedback to climate, part of the underestimated mid-Holocene temperature response to orbital forcing can be reconciled in the model.