Pacific warm pool subsurface heat sequestration modulated Walker circulation and ENSO activity during the Holocene-Reference-Cited by-同舟云学术

Pacific warm pool subsurface heat sequestration modulated Walker circulation and ENSO activity during the Holocene

Author:

Dang Haowen¹^ORCID,Jian Zhimin¹^ORCID,Wang Yue¹^ORCID,Mohtadi Mahyar²^ORCID,Rosenthal Yair³,Ye Liming⁴,Bassinot Franck⁵,Kuhnt Wolfgang⁶

Affiliation:

1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China.

2. MARUM-Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany.

3. Department of Marine and Coastal Science and Department of Earth and Planetary Sciences, Rutgers University, New Brunswick, NJ 08901, USA.

4. Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, Ministry of Natural Resources of China, Hangzhou 310012, China.

5. Laboratoire des Sciences du Climat et de l’Environnement/IPSL, CEA-CNRS-UVSQ, University Paris-Saclay, 91198 Gif-sur-Yvette, France.

6. Institute of Geosciences, Christian-Albrechts-University, D-24118 Kiel, Germany.

Abstract

Orbitally driven warm pool upper-water temperature regulates the equatorial Pacific climate change over the past 25,000 years.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference80 articles.

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