Sea-surface temperature reconstruction of the South China Sea
The tropical ocean plays a major role in global climate. It is therefore crucial to establish the precise phase between tropical and high-latitude climate variability during past abrupt climate events in order to gain insight into the mechanisms of global climate change. Here we present alkenone sea...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.738464 2023-05-15T16:29:02+02:00 Sea-surface temperature reconstruction of the South China Sea Kienast, Markus Steinke, Stephan Stattegger, Karl Calvert, Stephen E MEDIAN LATITUDE: 7.456567 * MEDIAN LONGITUDE: 110.026125 * SOUTH-BOUND LATITUDE: 5.663017 * WEST-BOUND LONGITUDE: 109.390767 * NORTH-BOUND LATITUDE: 9.250117 * EAST-BOUND LONGITUDE: 110.661483 * DATE/TIME START: 1996-12-17T00:00:00 * DATE/TIME END: 1996-12-30T00:00:00 2001-05-31 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.738464 https://doi.org/10.1594/PANGAEA.738464 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.738464 https://doi.org/10.1594/PANGAEA.738464 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Kienast, Markus; Steinke, Stephan; Stattegger, Karl; Calvert, Stephen E (2001): Synchronous tropical South China Sea SST change and Greenland warming during deglaciation. Science, 291(5511), 2132-2134, https://doi.org/10.1126/science.1057131 GIK18252-3 GIK18287-3 Gravity corer (Kiel type) SL SO115 SO115_05 SO115_40 Sonne SUNDAFLUT Sunda Shelf Vietnam shelf Dataset 2001 ftpangaea https://doi.org/10.1594/PANGAEA.738464 https://doi.org/10.1126/science.1057131 2023-01-20T07:31:48Z The tropical ocean plays a major role in global climate. It is therefore crucial to establish the precise phase between tropical and high-latitude climate variability during past abrupt climate events in order to gain insight into the mechanisms of global climate change. Here we present alkenone sea surface temperature (SST) records from the tropical South China Sea that show an abrupt temperature increase of at least 1°C at the end of the last glacial period. Within the recognized dating uncertainties, this SST increase is synchronous with the Bølling warming observed at 14.6 thousand years ago in the Greenland Ice Sheet Project 2 ice core. Dataset Greenland Greenland Ice Sheet Project ice core Ice Sheet PANGAEA - Data Publisher for Earth & Environmental Science Greenland Sunda ENVELOPE(-6.982,-6.982,62.205,62.205) ENVELOPE(109.390767,110.661483,9.250117,5.663017) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
GIK18252-3 GIK18287-3 Gravity corer (Kiel type) SL SO115 SO115_05 SO115_40 Sonne SUNDAFLUT Sunda Shelf Vietnam shelf |
spellingShingle |
GIK18252-3 GIK18287-3 Gravity corer (Kiel type) SL SO115 SO115_05 SO115_40 Sonne SUNDAFLUT Sunda Shelf Vietnam shelf Kienast, Markus Steinke, Stephan Stattegger, Karl Calvert, Stephen E Sea-surface temperature reconstruction of the South China Sea |
topic_facet |
GIK18252-3 GIK18287-3 Gravity corer (Kiel type) SL SO115 SO115_05 SO115_40 Sonne SUNDAFLUT Sunda Shelf Vietnam shelf |
description |
The tropical ocean plays a major role in global climate. It is therefore crucial to establish the precise phase between tropical and high-latitude climate variability during past abrupt climate events in order to gain insight into the mechanisms of global climate change. Here we present alkenone sea surface temperature (SST) records from the tropical South China Sea that show an abrupt temperature increase of at least 1°C at the end of the last glacial period. Within the recognized dating uncertainties, this SST increase is synchronous with the Bølling warming observed at 14.6 thousand years ago in the Greenland Ice Sheet Project 2 ice core. |
format |
Dataset |
author |
Kienast, Markus Steinke, Stephan Stattegger, Karl Calvert, Stephen E |
author_facet |
Kienast, Markus Steinke, Stephan Stattegger, Karl Calvert, Stephen E |
author_sort |
Kienast, Markus |
title |
Sea-surface temperature reconstruction of the South China Sea |
title_short |
Sea-surface temperature reconstruction of the South China Sea |
title_full |
Sea-surface temperature reconstruction of the South China Sea |
title_fullStr |
Sea-surface temperature reconstruction of the South China Sea |
title_full_unstemmed |
Sea-surface temperature reconstruction of the South China Sea |
title_sort |
sea-surface temperature reconstruction of the south china sea |
publisher |
PANGAEA |
publishDate |
2001 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.738464 https://doi.org/10.1594/PANGAEA.738464 |
op_coverage |
MEDIAN LATITUDE: 7.456567 * MEDIAN LONGITUDE: 110.026125 * SOUTH-BOUND LATITUDE: 5.663017 * WEST-BOUND LONGITUDE: 109.390767 * NORTH-BOUND LATITUDE: 9.250117 * EAST-BOUND LONGITUDE: 110.661483 * DATE/TIME START: 1996-12-17T00:00:00 * DATE/TIME END: 1996-12-30T00:00:00 |
long_lat |
ENVELOPE(-6.982,-6.982,62.205,62.205) ENVELOPE(109.390767,110.661483,9.250117,5.663017) |
geographic |
Greenland Sunda |
geographic_facet |
Greenland Sunda |
genre |
Greenland Greenland Ice Sheet Project ice core Ice Sheet |
genre_facet |
Greenland Greenland Ice Sheet Project ice core Ice Sheet |
op_source |
Supplement to: Kienast, Markus; Steinke, Stephan; Stattegger, Karl; Calvert, Stephen E (2001): Synchronous tropical South China Sea SST change and Greenland warming during deglaciation. Science, 291(5511), 2132-2134, https://doi.org/10.1126/science.1057131 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.738464 https://doi.org/10.1594/PANGAEA.738464 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.738464 https://doi.org/10.1126/science.1057131 |
_version_ |
1766018729132425216 |