Southern Ocean convection amplified past Antarctic warming and atmospheric CO2 rise during Heinrich Stadial 4

Antarctic warming and the rise of atmospheric CO2 levels during Heinrich Stadial 4 were amplified by enhanced convection and air-sea gas and heat exchange in the Southern Ocean, according to an analysis of deep water ventilation and temperature proxies

Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Luke Skinner, Laurie Menviel, Lauren Broadfield, Julia Gottschalk, Mervyn Greaves
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2020
Subjects:
Geology
QE1-996.5
Environmental sciences
GE1-350
Antarctic
Southern Ocean
Antarc*
Online Access:https://doi.org/10.1038/s43247-020-00024-3
https://doaj.org/article/cb8a51b537314a7abe0b32656b054377
Description
Summary:Antarctic warming and the rise of atmospheric CO2 levels during Heinrich Stadial 4 were amplified by enhanced convection and air-sea gas and heat exchange in the Southern Ocean, according to an analysis of deep water ventilation and temperature proxies

Similar Items