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  4. Australian shelf sediments reveal shifts in Miocene Southern Hemisphere westerlies
 
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Australian shelf sediments reveal shifts in Miocene Southern Hemisphere westerlies

Journal
Science Advances
Journal Volume
3
Journal Issue
5
Date Issued
2017
Author(s)
JEROEN GROENEVELD  
Henderiks J
Renema W
McHugh C.M
De Vleeschouwer D
Christensen B.A
Fulthorpe C.S
Reuning L
Gallagher S.J
Bogus K
Auer G
Ishiwa T
Expedition 356 Scientists
DOI
10.1126/sciadv.1602567
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85026292606&doi=10.1126%2fsciadv.1602567&partnerID=40&md5=9cbaac4eaa88bbf0da9b80ad7a00a8f5
https://scholars.lib.ntu.edu.tw/handle/123456789/624758
Abstract
Global climate underwent a major reorganization when the Antarctic ice sheet expanded ∼14 million years ago (Ma) (1). This event affected global atmospheric circulation, including the strength and position of the westerlies and the Intertropical Convergence Zone (ITCZ), and, therefore, precipitation patterns (2-5). We present new shallow-marine sediment records from the continental shelf of Australia (International Ocean Discovery Program Sites U1459 and U1464) providing the first empirical evidence linking high-latitude cooling around Antarctica to climate change in the (sub)tropics during the Miocene. We show that Western Australia was arid during most of the Middle Miocene. Southwest Australia became wetter during the Late Miocene, creating a climate gradient with the arid interior, whereas northwest Australia remained arid throughout. Precipitation and river runoff in southwest Australia gradually increased from 12 to 8 Ma, which we relate to a northward migration or intensification of the westerlies possibly due to increased sea ice in the Southern Ocean (5). Abrupt aridification indicates that the westerlies shifted back to a position south of Australia after 8 Ma. Our midlatitude Southern Hemisphere data are consistent with the inference that expansion of sea ice around Antarctica resulted in a northward movement of the westerlies. In turn, this may have pushed tropical atmospheric circulation and the ITCZ northward, shifting the main precipitation belt over large parts of Southeast Asia (4). © 2017 The Authors, some rights reserved.
Other Subjects
Climate change; Climatology; Meteorology; Sea ice; Sediments; Submarine geology; Antarctic ice sheets; Atmospheric circulation; Climate gradients; Continental shelves; Intertropical convergence zone; Precipitation patterns; Southern Hemisphere; Southwest australia; Ice; Antarctica; article; climate change; continental shelf; cooling; latitude; Middle Miocene; precipitation; river; runoff; sea ice; sediment; South Australia; Southeast Asia; Southern Hemisphere; Southern Ocean; tropics; Upper Miocene; Western Australia
Type
journal article

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