Reconstruction of Bering Strait volume transport suggesting the contribution of Bering Sea continental shelf to the pressure head forcing

The author reconstructed in-situ volume transport (VT) through the Bering Strait using the NNW wind component, the gradient of dynamic ocean topography (DOT) across the strait and DOT in the East Siberian Sea (RMSE = 0.2 Sv). The difference between in-situ VT and reconstructed VT (diffVT) was correl...

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Bibliographic Details
Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16411
http://id.nii.ac.jp/1291/00016289/