Reverse Estuarine Circulation Due to Local and Remote Wind Forcing, Enhanced by the Presence of Along‐Coast Estuaries-Reference-Cited by-同舟云学术

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Reverse Estuarine Circulation Due to Local and Remote Wind Forcing, Enhanced by the Presence of Along‐Coast Estuaries

Published:2017-12 Issue:12 Volume:122 Page:10184-10205
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Giddings S. N.¹^ORCID,MacCready P.²^ORCID

Affiliation:

1. Scripps Institution of OceanographyUniversity of California San DiegoLa Jolla CA USA

2. School of OceanographyUniversity of WashingtonSeattle WA USA

Funder

National Oceanic and Atmospheric Administration

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/10.1002/2016JC012479

Reference99 articles.

1. Maximal two-layer exchange through a contraction with barotropic net flow

2. Turnover times for the water above sill level in Gullmar Fjord

3. The rate of inflow and mixing during deep-water renewal in a sill fjord

4. Observations of inshore water exchange forced by a fluctuating offshore density field

5. Variation in the position of the upwelling front on the Oregon shelf

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