Mohtadi, Mahyar, Prange, Matthias, Schefuß, Enno and Jennerjahn, Tim C. (2017) Late Holocene slowdown of the Indian Ocean Walker circulation. Nature Communications, 8 (1). DOI https://doi.org/10.1038/s41467-017-00855-3.

[img] Text
Jennerjahn et al 2017a.pdf - Published Version
Restricted to Registered users only
Available under License Creative Commons: Attribution 4.0.

Download (1MB)

Abstract

Changes in tropical zonal atmospheric (Walker) circulation induce shifts in rainfall patterns along with devastating floods and severe droughts that dramatically impact the lives of millions of people. Historical records and observations of the Walker circulation over the 20th century disagree on the sign of change and therefore, longer climate records are necessary to better project tropical circulation changes in response to global warming. Here we examine proxies for thermocline depth and rainfall in the eastern tropical Indian Ocean during the globally colder Last Glacial Maximum (19–23 thousand years ago) and for the past 3000 years. We show that increased thermocline depth and rainfall indicate a stronger-than-today Walker circulation during the Last Glacial Maximum, which is supported by an ensemble of climate simulations. Our findings underscore the sensitivity of tropical circulation to temperature change and provide evidence for a further weakening of the Walker circulation in response to greenhouse warming.

Document Type: Article
Research affiliation: Biogeochemistry and Geology > Ecological Biogeochemistry
Refereed: Yes
Open Access Journal?: Yes
DOI etc.: https://doi.org/10.1038/s41467-017-00855-3
ISSN: 2041-1723
Date Deposited: 10 Apr 2019 11:18
Last Modified: 01 Oct 2020 12:58
URI: http://cris.leibniz-zmt.de/id/eprint/1745

Actions (login required)

View Item View Item