Effects of the Relaxation of Upwelling‐Favorable Winds on the Diurnal and Semidiurnal Water Temperature Fluctuations in the Santa Barbara Channel, California-Reference-Cited by-同舟云学术

Effects of the Relaxation of Upwelling‐Favorable Winds on the Diurnal and Semidiurnal Water Temperature Fluctuations in the Santa Barbara Channel, California

Published:2017-10 Issue:10 Volume:122 Page:7958-7977
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Aristizábal María F.¹²^ORCID,Fewings Melanie R.¹^ORCID,Washburn Libe³^ORCID

Affiliation:

1. Department of Marine SciencesUniversity of ConnecticutGroton CT USA

2. Now at NASA Goddard Institute for Space StudiesNew York NY USA

3. Marine Science Institute and Department of GeographyUniversity of CaliforniaSanta Barbara CA USA

Funder

National Science Foundation

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/10.1002/2017JC013199

Reference55 articles.

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2. Upwelling circulation on the Oregon continental shelf. Part I: Response to idealized forcing;Allen J. S.;Journal of Oceanography,1995

3. Contrasting spatial patterns in the diurnal and semidiurnal temperature variability in the Santa Barbara Channel, California

4. The low-frequency transport in the Santa Barbara Channel: description and forcing

5. The inner shelf response to wind‐driven upwelling and downwelling;Austin J. A.;Journal of Oceanography,2002

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