CP Climate of the Past CP Clim. Past 1814-9332 Copernicus Publications Göttingen, Germany 10.5194/cp-4-59-2008 Detecting vegetation-precipitation feedbacks in mid-Holocene North Africa from two climate models Wang Y. 1 3 Notaro M. 1 Liu Z. 1 Gallimore R. 1 Levis S. 2 Kutzbach J. E. 1 Center for Climatic Research, University of Wisconsin-Madison, 1225 West Dayton Street, Madison, WI 53706, USA National Center for Atmospheric Research, PO BOX 3000, Boulder, CO 80307, USA now at: Pacific Northwest National Laboratory, PO BOX 999, MSIN K9-24, Richland, WA 99352, USA 31 03 2008 4 1 59 67 Copyright: © 2008 Y. Wang et al. 2008 This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/3.0/ This article is available from https://cp.copernicus.org/articles/4/59/2008/cp-4-59-2008.html The full text article is available as a PDF file from https://cp.copernicus.org/articles/4/59/2008/cp-4-59-2008.pdf

Using two climate-vegetation model simulations from the Fast Ocean Atmosphere Model (FOAM) and the Community Climate System Model (CCSM, version 2), we investigate vegetation-precipitation feedbacks across North Africa during the mid-Holocene. From mid-Holocene snapshot runs of FOAM and CCSM2, we detect a negative feedback at the annual timescale with our statistical analysis. Using the Monte-Carlo bootstrap method, the annual negative feedback is further confirmed to be significant in both simulations. Additional analysis shows that this negative interaction is partially caused by the competition between evaporation and transpiration in North African grasslands. Furthermore, we find the feedbacks decrease with increasing timescales, and change signs from positive to negative at increasing timescales in FOAM. The proposed mechanism for this sign switch is associated with the different persistent timescales of upper and lower soil water contents, and their interactions with vegetation and atmospheric precipitation.

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