Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation ...
Ocean-atmosphere interactions in the tropical Pacific region have a strong influence on global heat and water vapour transport and thus constitute an important component of the climate system1,2. Changes in sea surface temperatures and convection in the tropical Indo-Pacific region are thought to be...
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ftdatacite:10.1594/pangaea.898714 2024-09-15T17:47:13+00:00 Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation ... Visser, Katherine Thunell, Robert C Stott, Lowell D 2019 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.898714 https://doi.pangaea.de/10.1594/PANGAEA.898714 en eng PANGAEA https://dx.doi.org/10.1038/nature01297 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Deglaciation Indonesia Mg/Ca Pacific Warm Pool SST DEPTH, sediment/rock AGE Globigerinoides ruber, δ18O Globigerinoides ruber, Magnesium/Calcium ratio Sea surface temperature Calypso Corer Calculated from Mg/Ca ratios Anand et al., 2003 Calculated from Mg/Ca ratios Lea et al. 2000 MD111 Marion Dufresne 1995 dataset Supplementary Dataset Dataset 2019 ftdatacite https://doi.org/10.1594/pangaea.89871410.1038/nature01297 2024-08-01T10:53:02Z Ocean-atmosphere interactions in the tropical Pacific region have a strong influence on global heat and water vapour transport and thus constitute an important component of the climate system1,2. Changes in sea surface temperatures and convection in the tropical Indo-Pacific region are thought to be responsible for the interannual to decadal climate variability observed in extratropical regions1,3, but the role of the tropics in climate changes on millennial and orbital timescales is less clear. Here we analyse oxygen isotopes and Mg/Ca ratios of foraminiferal shells from the Makassar strait in the heart of the Indo-Pacific warm pool, to obtain synchronous estimates of sea surface temperatures and ice volume. We find that sea surface temperatures increased by 3.5-4.0 8C during the last two glacial—interglacial transitions, synchronous with the global increase in atmospheric CO2 and Antarctic warming, but the temperature increase occurred 2,000- 3,000 years before the Northern Hemisphere ice sheets melted. ... : Supplement to: Visser, Katherine; Thunell, Robert C; Stott, Lowell D (2003): Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation. Nature, 421(6919), 152-155 ... Dataset Antarc* Antarctic DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Deglaciation Indonesia Mg/Ca Pacific Warm Pool SST DEPTH, sediment/rock AGE Globigerinoides ruber, δ18O Globigerinoides ruber, Magnesium/Calcium ratio Sea surface temperature Calypso Corer Calculated from Mg/Ca ratios Anand et al., 2003 Calculated from Mg/Ca ratios Lea et al. 2000 MD111 Marion Dufresne 1995 |
spellingShingle |
Deglaciation Indonesia Mg/Ca Pacific Warm Pool SST DEPTH, sediment/rock AGE Globigerinoides ruber, δ18O Globigerinoides ruber, Magnesium/Calcium ratio Sea surface temperature Calypso Corer Calculated from Mg/Ca ratios Anand et al., 2003 Calculated from Mg/Ca ratios Lea et al. 2000 MD111 Marion Dufresne 1995 Visser, Katherine Thunell, Robert C Stott, Lowell D Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation ... |
topic_facet |
Deglaciation Indonesia Mg/Ca Pacific Warm Pool SST DEPTH, sediment/rock AGE Globigerinoides ruber, δ18O Globigerinoides ruber, Magnesium/Calcium ratio Sea surface temperature Calypso Corer Calculated from Mg/Ca ratios Anand et al., 2003 Calculated from Mg/Ca ratios Lea et al. 2000 MD111 Marion Dufresne 1995 |
description |
Ocean-atmosphere interactions in the tropical Pacific region have a strong influence on global heat and water vapour transport and thus constitute an important component of the climate system1,2. Changes in sea surface temperatures and convection in the tropical Indo-Pacific region are thought to be responsible for the interannual to decadal climate variability observed in extratropical regions1,3, but the role of the tropics in climate changes on millennial and orbital timescales is less clear. Here we analyse oxygen isotopes and Mg/Ca ratios of foraminiferal shells from the Makassar strait in the heart of the Indo-Pacific warm pool, to obtain synchronous estimates of sea surface temperatures and ice volume. We find that sea surface temperatures increased by 3.5-4.0 8C during the last two glacial—interglacial transitions, synchronous with the global increase in atmospheric CO2 and Antarctic warming, but the temperature increase occurred 2,000- 3,000 years before the Northern Hemisphere ice sheets melted. ... : Supplement to: Visser, Katherine; Thunell, Robert C; Stott, Lowell D (2003): Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation. Nature, 421(6919), 152-155 ... |
format |
Dataset |
author |
Visser, Katherine Thunell, Robert C Stott, Lowell D |
author_facet |
Visser, Katherine Thunell, Robert C Stott, Lowell D |
author_sort |
Visser, Katherine |
title |
Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation ... |
title_short |
Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation ... |
title_full |
Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation ... |
title_fullStr |
Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation ... |
title_full_unstemmed |
Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation ... |
title_sort |
magnitude and timing of temperature change in the indo-pacific warm pool during deglaciation ... |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://dx.doi.org/10.1594/pangaea.898714 https://doi.pangaea.de/10.1594/PANGAEA.898714 |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
https://dx.doi.org/10.1038/nature01297 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.89871410.1038/nature01297 |
_version_ |
1810496097565540352 |