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020 ▼a 9780438103283
035 ▼a (MiAaPQ)AAI10826160
035 ▼a (MiAaPQ)ucsd:17549
040 ▼a MiAaPQ ▼c MiAaPQ ▼d 247004
0820 ▼a 551.46
1001 ▼a Rocha, Cesar Barbedo.
24514 ▼a The Turbulent and Wavy Upper Ocean: Transition from Geostrophic Flows to Internal Waves and Stimulated Generation of Near-inertial Waves.
260 ▼a [S.l.]: ▼b University of California, San Diego., ▼c 2018.
260 1 ▼a Ann Arbor: ▼b ProQuest Dissertations & Theses, ▼c 2018.
300 ▼a 234 p.
500 ▼a Source: Dissertation Abstracts International, Volume: 79-11(E), Section: B.
500 ▼a Adviser: William R. Young.
5021 ▼a Thesis (Ph.D.)--University of California, San Diego, 2018.
520 ▼a We study the mesoscale to submesoscale (10-300 km) dynamics of the upper ocean, with particular attention to the partitioning between geostrophic flows and internal waves, and the interaction between these two types of flow. Using 13 years of sh
520 ▼a The observational and modeling evidence of the importance of both geostrophic flows and internal gravity waves at mesoscales to submesoscales hints on the interaction between these two types of flow. To better understand these interactions, we a
520 ▼a In a separate study, we derive a Galerkin approximation for the surface-active quasi-geostrophic system using standard vertical modes. While the Galerkin expansions of streamfunction and potential vorticity do not satisfy the inversion relation
590 ▼a School code: 0033.
650 4 ▼a Physical oceanography.
690 ▼a 0415
71020 ▼a University of California, San Diego. ▼b Oceanography.
7730 ▼t Dissertation Abstracts International ▼g 79-11B(E).
773 ▼t Dissertation Abstract International
790 ▼a 0033
791 ▼a Ph.D.
792 ▼a 2018
793 ▼a English
85640 ▼u http://www.riss.kr/pdu/ddodLink.do?id=T14998851 ▼n KERIS ▼z 이 자료의 원문은 한국교육학술정보원에서 제공합니다.
980 ▼a 201812 ▼f 2019
990 ▼a ***1012033