Anisotropic response of surface circulation to wind forcing, as inferred from high‐frequency radar currents in the southeastern B ay of B iscay-Reference-Cited by-同舟云学术

Anisotropic response of surface circulation to wind forcing, as inferred from high‐frequency radar currents in the southeastern B ay of B iscay

Published:2015-04 Issue:4 Volume:120 Page:2945-2957
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Fontán Almudena¹,Cornuelle Bruce²

Affiliation:

1. Marine Research Division, AZTI‐TecnaliaPasaia Spain

2. Department of Climate, Atmospheric Science and Physical OceanographyScripps Institution of Oceanography, University of CaliforniaSan Diego California USA

Funder

Ministry of Economy and Competitiveness through the project

Department of Economic Development and Competitiveness of the Basque Government

NOAA

National Science Foundation (NSF)

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2014JC010671

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4. Seasonal differences in wind-driven across-shelf forcing and response relationships in the shelf surface layer of the central Mid-Atlantic Bight

5. On the influence of the Earth's rotation on ocean‐currents;Ekman V.;Ark. Mat. Astron. Fysik,1905

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