Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle
A comparison of glacial advances through the last glacial cycle between Northern and Southern Hemispheres in the PEP 2 transect (East Asia and Australasia) revealed (1) a relatively good synchrony of glacial advances during the LGM across the whole transect except Antarctica, (2) a rough synchrony i...
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ftunivqespace:oai:espace.library.uq.edu.au:UQ:190900 2023-05-15T13:55:31+02:00 Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle Ono, Yugo Shulmeister, James Lemkuhle, Frank Asahi, Katsuhiko Aoki, Tatsuto 2004-01-01 https://espace.library.uq.edu.au/view/UQ:190900 eng eng Pergamon Press doi:10.1016/S1040-6182(03)00130-7 issn:1040-6182 orcid:0000-0001-5863-9462 late quaternary glaciations new-zealand northern pakistan tibetan plateau lahul-himalaya paleoenvironmental change southwest pacific western mongolia late pleistocene summer monsoon 040104 Climate Change Processes Journal Article 2004 ftunivqespace https://doi.org/10.1016/S1040-6182(03)00130-7 2020-10-27T00:28:23Z A comparison of glacial advances through the last glacial cycle between Northern and Southern Hemispheres in the PEP 2 transect (East Asia and Australasia) revealed (1) a relatively good synchrony of glacial advances during the LGM across the whole transect except Antarctica, (2) a rough synchrony in glacial advances in the Karakorums, Himalayas, Japan, and New Zealand during Marine Isotope Stages (MIS) 3 and 4, although the age control is still poor, and (1) a greater glacial extent in MIS 3 and 4 than in MIS 2. The LGM advances are driven by Northern Hemisphere temperature forcing, but the MIS 3 and/or MIS 4 advances appear to be dominantly controlled by the effects of moisture availability or lack of thereof. In mainland Australia and Antarctica glaciers advanced only in the most humid phases. In Himalaya and Karakorum, where the moisture is supplied both by a Summer monsoon and the westerlies, timings of glacier advance coincide with both Summer monsoon enhancement and westerly intensification. In Japan the glacier extent is controlled by monsoon changes, sea-surface temperatures (SSTs) in the Japan Sea (moisture source) and by zonal shifts in westerly circulation. In New Zealand, either insolalion changes or changes in the intensity of westerly circulation are invoked, Lis the main track of the westerlies did not change greatly during glacial times. (C) 2003 Elsevier Ltd and INQUA. All rights reserved. Article in Journal/Newspaper Antarc* Antarctica The University of Queensland: UQ eSpace New Zealand Pacific Quaternary International 118-119 55 68 |
institution |
Open Polar |
collection |
The University of Queensland: UQ eSpace |
op_collection_id |
ftunivqespace |
language |
English |
topic |
late quaternary glaciations new-zealand northern pakistan tibetan plateau lahul-himalaya paleoenvironmental change southwest pacific western mongolia late pleistocene summer monsoon 040104 Climate Change Processes |
spellingShingle |
late quaternary glaciations new-zealand northern pakistan tibetan plateau lahul-himalaya paleoenvironmental change southwest pacific western mongolia late pleistocene summer monsoon 040104 Climate Change Processes Ono, Yugo Shulmeister, James Lemkuhle, Frank Asahi, Katsuhiko Aoki, Tatsuto Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle |
topic_facet |
late quaternary glaciations new-zealand northern pakistan tibetan plateau lahul-himalaya paleoenvironmental change southwest pacific western mongolia late pleistocene summer monsoon 040104 Climate Change Processes |
description |
A comparison of glacial advances through the last glacial cycle between Northern and Southern Hemispheres in the PEP 2 transect (East Asia and Australasia) revealed (1) a relatively good synchrony of glacial advances during the LGM across the whole transect except Antarctica, (2) a rough synchrony in glacial advances in the Karakorums, Himalayas, Japan, and New Zealand during Marine Isotope Stages (MIS) 3 and 4, although the age control is still poor, and (1) a greater glacial extent in MIS 3 and 4 than in MIS 2. The LGM advances are driven by Northern Hemisphere temperature forcing, but the MIS 3 and/or MIS 4 advances appear to be dominantly controlled by the effects of moisture availability or lack of thereof. In mainland Australia and Antarctica glaciers advanced only in the most humid phases. In Himalaya and Karakorum, where the moisture is supplied both by a Summer monsoon and the westerlies, timings of glacier advance coincide with both Summer monsoon enhancement and westerly intensification. In Japan the glacier extent is controlled by monsoon changes, sea-surface temperatures (SSTs) in the Japan Sea (moisture source) and by zonal shifts in westerly circulation. In New Zealand, either insolalion changes or changes in the intensity of westerly circulation are invoked, Lis the main track of the westerlies did not change greatly during glacial times. (C) 2003 Elsevier Ltd and INQUA. All rights reserved. |
format |
Article in Journal/Newspaper |
author |
Ono, Yugo Shulmeister, James Lemkuhle, Frank Asahi, Katsuhiko Aoki, Tatsuto |
author_facet |
Ono, Yugo Shulmeister, James Lemkuhle, Frank Asahi, Katsuhiko Aoki, Tatsuto |
author_sort |
Ono, Yugo |
title |
Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle |
title_short |
Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle |
title_full |
Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle |
title_fullStr |
Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle |
title_full_unstemmed |
Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle |
title_sort |
timings and causes of glacial advances across the pep-ii transect (east-asia to antarctica) during the last glaciation cycle |
publisher |
Pergamon Press |
publishDate |
2004 |
url |
https://espace.library.uq.edu.au/view/UQ:190900 |
geographic |
New Zealand Pacific |
geographic_facet |
New Zealand Pacific |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
doi:10.1016/S1040-6182(03)00130-7 issn:1040-6182 orcid:0000-0001-5863-9462 |
op_doi |
https://doi.org/10.1016/S1040-6182(03)00130-7 |
container_title |
Quaternary International |
container_volume |
118-119 |
container_start_page |
55 |
op_container_end_page |
68 |
_version_ |
1766262184493449216 |