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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Bibliographic Details
Main Authors: Kyung Eun Lee, Steven C. Clemens, Yoshimi Kubota, Axel Timmermann, Ann Holbourn, Sang-Wook Yeh, Si Woong Bae, Tae Wook Ko
Format: article
Language:EN
Published: Nature Portfolio 2021
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Online Access:https://doaj.org/article/e3b90491ea9a4529ad29be14961b87dd
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