Paleo‐ocean Destratification Triggered by the Subduction of the Oyashio Water Into the Sea of Japan After the Last Glacial Maximum-Reference-Cited by-同舟云学术

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Paleo‐ocean Destratification Triggered by the Subduction of the Oyashio Water Into the Sea of Japan After the Last Glacial Maximum

Published:2020-03 Issue:3 Volume:35 Page:
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanography and Paleoclimatology

Author:

Isobe Atsuhiko¹^ORCID

Affiliation:

1. Research Institute for Applied MechanicsKyushu University Kasuga Japan

Funder

Japan Society for the Promotion of Science

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019PA003593

Reference43 articles.

1. Numerical simulation of ice-ocean variability in the Barents Sea region

2. A 36 kyr geochemical record from the Sea of Japan of organic matter flux variations and changes in intermediate water oxygen concentrations

3. Impact of model resolution on Arctic sea ice and North Atlantic Ocean heat transport

4. A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation

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1. North-south discrepancy in the contributors to CB153 accumulation in the deep water of the Sea of Japan;Science of The Total Environment;2024-08

2. Global sea level controlled the deep low-salinity pool evolution in the Japan sea since the last glacial period;Quaternary Science Reviews;2024-03

3. North-South Discrepancy in the Contributors to Cb153 Accumulation in the Deep Water of the Sea of Japan;2024

4. Diagnostic Analysis of the Response of Volume Transport through the Tsushima Strait to the Eddy-Induced Variations in the Kuroshio Region;Journal of Physical Oceanography;2023-11

5. Low Sea Surface Salinity Event of the Japan Sea During the Last Glacial Maximum;Paleoceanography and Paleoclimatology;2023-01

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