Stability of a Flow Over Bottom Topography: A General Condition and a Linear Analysis in a Two‐Layer Quasi‐Geostrophic Model With a Possible Application to a Kuroshio Meander-Reference-Cited by-同舟云学术

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Stability of a Flow Over Bottom Topography: A General Condition and a Linear Analysis in a Two‐Layer Quasi‐Geostrophic Model With a Possible Application to a Kuroshio Meander

Published:2021-12 Issue:12 Volume:126 Page:
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:JGR Oceans

Author:

Tanaka Yuki¹^ORCID

Affiliation:

1. Faculty of Marine Science and Technology Fukui Prefectural University Obama Japan

Funder

Japan Society for the Promotion of Science

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/10.1029/2021JC017849

Reference58 articles.

1. Transition to the large meander path of the Kuroshio as observed by satellite altimetry;Ambe D.;La Mer,2009

2. Conditions for non‐linear stability of stationary plane curvilinear flows of an ideal fluid;Arnold V. I.;Doklady Akademii Nauk SSSR,1965

3. On an a priori estimate in the theory of hydrodynamic stability;Arnold V. I.;Izvestiya Vysshikh Uchebnykh Zavedenii, Matematika,1966

4. Destabilization of barotropic flows small-scale topography

5. On Spectral Analysis of Mesoscale Eddies. Part I: Linear Analysis

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