Semidiurnal internal tide energy fluxes and their variability in a G lobal O cean M odel and moored observations-Reference-Cited by-同舟云学术

Semidiurnal internal tide energy fluxes and their variability in a G lobal O cean M odel and moored observations

Published:2017-03 Issue:3 Volume:122 Page:1882-1900
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Ansong Joseph K.¹^ORCID,Arbic Brian K.¹^ORCID,Alford Matthew H.²^ORCID,Buijsman Maarten C.³^ORCID,Shriver Jay F.⁴,Zhao Zhongxiang⁵,Richman James G.⁶^ORCID,Simmons Harper L.⁷,Timko Patrick G.⁸^ORCID,Wallcraft Alan J.⁴,Zamudio Luis⁶

Affiliation:

1. Department of Earth and Environmental SciencesUniversity of MichiganAnn Arbor Michigan USA

2. Scripps Institution of Oceanography, University of CaliforniaSan Diego, San Diego California USA

3. Department of Marine ScienceUniversity of Southern Mississippi Mississippi USA

4. Ocean Dynamics and Prediction Branch, Code 7323Naval Research Laboratory Mississippi USA

5. Applied Physics Laboratory and School of OceanographySeattle Washington USA

6. Center for Ocean and Atmospheric PredictionFlorida State UniversityTallahassee Florida USA

7. International Arctic Research CenterUniversity of Alaska‐FairbanksFairbanks Alaska USA

8. Centre for Applied Marine SciencesBangor UniversityMenai Bridge Anglesey UK

Funder

National Science Foundation

Office of Naval Research

Department of Defense

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/10.1002/2016JC012184

Reference70 articles.

1. Global Patterns of Low-Mode Internal-Wave Propagation. Part I: Energy and Energy Flux

2. Internal waves across the Pacific

3. The formation and fate of internal waves in the South China Sea

4. Indirect evidence for substantial damping of low‐mode internal tides in the open ocean

5. The accuracy of surface elevations in forward global barotropic and baroclinic tide models

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