Sea surface temperatures from the Western Pacific Warm Pool across the last 17kyrs

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Main Authors: Moffa-Sanchez, Paola, Rosenthal, Yair, Babila, Tali L, Mohtadi, Mahyar, Zhang, Xu
Format: Dataset Open Access
Language:en
Published: PANGAEA 2019
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author Moffa-Sanchez, Paola
Rosenthal, Yair
Babila, Tali L
Mohtadi, Mahyar
Zhang, Xu
author_facet Moffa-Sanchez, Paola
Rosenthal, Yair
Babila, Tali L
Mohtadi, Mahyar
Zhang, Xu
collection Datos científicos de ciencias marinas y ambientales
contents The Indo-Pacific Warm Pool (IPWP) contains the warmest surface ocean waters on our planet. Changes in the extent and position of the IPWP likely impacted the tropical and global climate in the past. To put recent ocean changes into a longer temporal context, we present new paleoceanographic sea surface temperature reconstructions from off Papua New Guinea (RR1313-23PC: 4.4939°S, 145.6703°E, 712 m water depth) which is at the heart of the Western Pacific Warm Pool (WPWP), which is the warmest region within the IPWP, across the last 17,000 years. A new surface temperature dataset from the northeast South China Sea is also presented (ODP1144: 20.053°N, 117.4189°E; water depth 2037 m). In both locations we use Mg/Ca measurements on G.ruber s.s. (white) to calculate sea surface temperatures.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_902662
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Sea surface temperatures from the Western Pacific Warm Pool across the last 17kyrs
Moffa-Sanchez, Paola
Rosenthal, Yair
Babila, Tali L
Mohtadi, Mahyar
Zhang, Xu
G.ruber; Holocene; Mg/Ca; Western Pacific
The Indo-Pacific Warm Pool (IPWP) contains the warmest surface ocean waters on our planet. Changes in the extent and position of the IPWP likely impacted the tropical and global climate in the past. To put recent ocean changes into a longer temporal context, we present new paleoceanographic sea surface temperature reconstructions from off Papua New Guinea (RR1313-23PC: 4.4939°S, 145.6703°E, 712 m water depth) which is at the heart of the Western Pacific Warm Pool (WPWP), which is the warmest region within the IPWP, across the last 17,000 years. A new surface temperature dataset from the northeast South China Sea is also presented (ODP1144: 20.053°N, 117.4189°E; water depth 2037 m). In both locations we use Mg/Ca measurements on G.ruber s.s. (white) to calculate sea surface temperatures.
title Sea surface temperatures from the Western Pacific Warm Pool across the last 17kyrs
topic G.ruber; Holocene; Mg/Ca; Western Pacific
url https://doi.org/10.1594/PANGAEA.902662