Subsurface Heat Channel Drove Sea Surface Warming in the High‐Latitude North Atlantic During the Mid‐Pleistocene Transition-Reference-Cited by-同舟云学术

Subsurface Heat Channel Drove Sea Surface Warming in the High‐Latitude North Atlantic During the Mid‐Pleistocene Transition

Published:2021-06-07 Issue:11 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

Catunda M. Carolina A.¹^ORCID,Bahr André¹^ORCID,Kaboth‐Bahr Stefanie¹²^ORCID,Zhang Xu³⁴^ORCID,Foukal Nicholas P.⁵^ORCID,Friedrich Oliver¹^ORCID

Affiliation:

1. Institute of Earth Sciences Heidelberg University Heidelberg Germany

2. Institute of Geosciences University of Potsdam Potsdam‐Golm Germany

3. Key Laboratory of Western China's Environmental Systems (Ministry of Education) College of Earth and Environmental Science Lanzhou University Lanzhou China

4. CAS Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences Beijing China

5. Department of Physical Oceanography Woods Hole Oceanographic Institution Woods Hole MA USA

Funder

Deutsche Forschungsgemeinschaft

Universität Potsdam

Lanzhou University

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL091899

Reference86 articles.

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5. Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present

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