Variations of the Somali upwelling since 18.5 ka BP and its relationship with southwest monsoon rainfall
<p>Somali upwelling history has been reconstructed for the last 18.5 ka BP based on biogenic silica fluxes estimated from a sediment core retrieved from the western Arabian Sea. Surface winds along the east African coast during the southwest monsoon (SWM) cause the Som...
Main Authors: | , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-09-01
|
Series: | Climate of the Past |
Online Access: | https://www.clim-past.net/14/1331/2018/cp-14-1331-2018.pdf |