Glacial Changes in Tropical Climate Amplified by the Indian Ocean

TitleGlacial Changes in Tropical Climate Amplified by the Indian Ocean
Publication TypeJournal Article
Year of Publication2018
JournalScience Advances
Volume4
Number12
Pageseaat9658
Date Published12/2018
Abstract

The mechanisms driving glacial-interglacial changes in the climate of the Indo-Pacific warm pool are poorly understood. Here we address this question combining paleoclimate proxies with model simulations of Last Glacial Maximum climate. We find evidence of two mechanisms explaining key patterns of ocean cooling and rainfall change interpreted from proxy data. Exposure of the Sahul shelf excites a positive ocean-atmosphere feedback involving a stronger surface temperature gradient along the equatorial Indian Ocean and a weaker Walker circulation – a response explaining the drier/wetter dipole across the basin. Northern hemisphere cooling by ice sheet albedo drives a monsoonal retreat across Africa and the Arabian Peninsula – a response that triggers a weakening of the Indian monsoon via cooling of the Arabian Sea and associated reductions in moisture supply. These results demonstrate the importance of air-sea interactions in the Indian Ocean amplifying externally-forced climate changes over a large part of the tropics.

URLhttp://dx.doi.org/10.1126/sciadv.aat9658
DOI10.1126/sciadv.aat9658
Journal: Science Advances
Number: 12
Volume: 4

The mechanisms driving glacial-interglacial changes in the climate of the Indo-Pacific warm pool are poorly understood. Here we address this question combining paleoclimate proxies with model simulations of Last Glacial Maximum climate. We find evidence of two mechanisms explaining key patterns of ocean cooling and rainfall change interpreted from proxy data. Exposure of the Sahul shelf excites a positive ocean-atmosphere feedback involving a stronger surface temperature gradient along the equatorial Indian Ocean and a weaker Walker circulation – a response explaining the drier/wetter dipole across the basin. Northern hemisphere cooling by ice sheet albedo drives a monsoonal retreat across Africa and the Arabian Peninsula – a response that triggers a weakening of the Indian monsoon via cooling of the Arabian Sea and associated reductions in moisture supply. These results demonstrate the importance of air-sea interactions in the Indian Ocean amplifying externally-forced climate changes over a large part of the tropics.

DOI: 10.1126/sciadv.aat9658
Year of Publication: 2018
Citation:
DiNezio, PN, JE Tierney, BL Otto-Bliesner, A Timmermann, T Bhattacharya, N Rosenbloom, and E Brady.  2018.  "Glacial Changes in Tropical Climate Amplified by the Indian Ocean."  Science Advances 4(12): eaat9658, doi:10.1126/sciadv.aat9658.