| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6446746 | Quaternary Science Reviews | 2013 | 14 Pages |
Abstract
⺠4 E-Socotran speleothems record the evolution of the NE monsoon over the last 7 ka. ⺠NE monsoon dries from 7 to 3.8 ka and remains stable afterwards. ⺠The local wettening of W-Socotra could relate to a change in SW wind path. ⺠N-Oman and E-Socotra are both influenced by the NE monsoon since 6 ka. ⺠Records currently located outside the ITCZ belt display an abrupt drying at 6 ka.
Related Topics
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Earth and Planetary Sciences
Geology
Authors
Maïté Van Rampelbergh, Dominik Fleitmann, Sophie Verheyden, Hai Cheng, Lawrence Edwards, Peter De Geest, David De Vleeschouwer, Stephen J. Burns, Albert Matter, Philippe Claeys, Eddy Keppens,