Roles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures

How temperatures at different seasons differ in response to different forcings is not well known. Here, the authors reconstruct annual and seasonal sea surface temperatures in the East China Sea and show that they react differently to CO2 and insolation forcing on glacial-interglacial timescales.

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Autores principales:	Kyung Eun Lee, Steven C. Clemens, Yoshimi Kubota, Axel Timmermann, Ann Holbourn, Sang-Wook Yeh, Si Woong Bae, Tae Wook Ko
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/e3b90491ea9a4529ad29be14961b87dd
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spelling	oai:doaj.org-article:e3b90491ea9a4529ad29be14961b87dd2021-12-02T17:37:42ZRoles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures10.1038/s41467-021-26051-y2041-1723https://doaj.org/article/e3b90491ea9a4529ad29be14961b87dd2021-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-26051-yhttps://doaj.org/toc/2041-1723How temperatures at different seasons differ in response to different forcings is not well known. Here, the authors reconstruct annual and seasonal sea surface temperatures in the East China Sea and show that they react differently to CO2 and insolation forcing on glacial-interglacial timescales.Kyung Eun LeeSteven C. ClemensYoshimi KubotaAxel TimmermannAnn HolbournSang-Wook YehSi Woong BaeTae Wook KoNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-13 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Kyung Eun Lee Steven C. Clemens Yoshimi Kubota Axel Timmermann Ann Holbourn Sang-Wook Yeh Si Woong Bae Tae Wook Ko Roles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures
description	How temperatures at different seasons differ in response to different forcings is not well known. Here, the authors reconstruct annual and seasonal sea surface temperatures in the East China Sea and show that they react differently to CO2 and insolation forcing on glacial-interglacial timescales.
format	article
author	Kyung Eun Lee Steven C. Clemens Yoshimi Kubota Axel Timmermann Ann Holbourn Sang-Wook Yeh Si Woong Bae Tae Wook Ko
author_facet	Kyung Eun Lee Steven C. Clemens Yoshimi Kubota Axel Timmermann Ann Holbourn Sang-Wook Yeh Si Woong Bae Tae Wook Ko
author_sort	Kyung Eun Lee
title	Roles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures
title_short	Roles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures
title_full	Roles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures
title_fullStr	Roles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures
title_full_unstemmed	Roles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures
title_sort	roles of insolation forcing and co2 forcing on late pleistocene seasonal sea surface temperatures
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/e3b90491ea9a4529ad29be14961b87dd
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Roles of insolation forcing and CO2 forcing on Late Pleistocene seasonal sea surface temperatures

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