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Comment on "Climate-driven ecosystem succession in the Sahara: the past 6000 years"
Victor Brovkin1, Martin Claussen
1Max Planck Institute for Meteorology, Bundesstrasse 55, 20146 Hamburg, Germany. victor.brovkin@zmaw.de
Abstract:
Kröpelin et al. (Research Articles, 9 May 2008, p. 765) interpreted a sediment record from Lake Yoa in the east-central part of North Africa as support for a weak biogeophysical climate-vegetation feedback in the Sahara during the mid-Holocene. We argue that the new data do not invalidate earlier modeling results on strong land-atmosphere coupling in the Western Sahara for which the Lake Yoa record is far less representative.
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