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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Main Authors: Kienast, Markus, Steinke, Stephan, Stattegger, Karl, Calvert, Stephen E
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
SL
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.738464
https://doi.org/10.1594/PANGAEA.738464
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.738464
record_format openpolar
spelling 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
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