Articles | Volume 12, issue 1
Clim. Past, 12, 51–73, 2016
https://doi.org/10.5194/cp-12-51-2016
Clim. Past, 12, 51–73, 2016
https://doi.org/10.5194/cp-12-51-2016

Research article 18 Jan 2016

Research article | 18 Jan 2016

Terrestrial biosphere changes over the last 120 kyr

B. A. A. Hoogakker et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (22 Sep 2015) by Hubertus Fischer
AR by Babette Hoogakker on behalf of the Authors (01 Oct 2015)  Author's response
ED: Reconsider after major revisions (15 Oct 2015) by Hubertus Fischer
AR by Babette Hoogakker on behalf of the Authors (30 Nov 2015)  Author's response    Manuscript
ED: Publish as is (14 Dec 2015) by Hubertus Fischer
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Short summary
In this paper we use two climate models to test how Earth’s vegetation responded to changes in climate over the last 120 000 years, looking at warm interglacial climates like today, cold ice-age glacial climates, and intermediate climates. The models agree well with observations from pollen, showing smaller forested areas and larger desert areas during cold periods. Forests store most terrestrial carbon; the terrestrial carbon lost during cold climates was most likely relocated to the oceans.