Thermal evolution of the western South Atlantic and the adjacent continent during Termination 1
During Termination 1, millennial-scale weakening events of the Atlantic meridional overturning circulation (AMOC) supposedly produced major changes in sea surface temperatures (SSTs) of the western South Atlantic, and in mean air temperatures (MATs) over southeastern South America. It has been sugge...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2015-06-01
|
| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/11/915/2015/cp-11-915-2015.pdf |