Abstract
The abrupt desertification over the northern Africa in the mid-Holocene is studied in both a complex and a simple coupled climate-vegetation model. In contrast to the previous mechanism that relies on strong positive vegetation-climate feedback and the resulted multiple equilibria, we propose a new mechanism in which the abrupt desertification is caused by low frequency climate variability, rather than a positive vegetation-climate feedback. The implication of this new mechanism to modelling and observation is also discussed.
Original language | English |
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Article number | L22709 |
Pages (from-to) | 1-6 |
Number of pages | 6 |
Journal | Geophysical Research Letters |
Volume | 33 |
Issue number | 22 |
DOIs | |
Publication status | Published - 28 Nov 2006 |
Externally published | Yes |