Linear Baroclinic Instability
Linear Baroclinic Instability is a theoretical framework in atmospheric and oceanic dynamics that describes the growth of small-amplitude perturbations in a baroclinic shear flow through linearized equations of motion, distinguishing it from nonlinear or finite-amplitude instability mechanisms by focusing exclusively on the initial exponential growth phase governed by linear dynamics.
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Ilson Carlos Almeida da Silveira, José Antônio Moreira Lima, André Campos Kersten Schmidt et al. · Dynamics of Atmospheres and Oceans · 2008 · 161 citations · Full text
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Chinese Academy of Sciences
Beijing, China
7 h-index
11 publications
311 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
7 publications
135 citations

NSF National Center for Atmospheric Research
Boulder, United States
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300 citations
Met Office
Exeter, United Kingdom
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5 publications
63 citations
Institute of Atmospheric Physics
Beijing, China
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110 citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
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4 publications
165 citations

Scripps Institution of Oceanography
La Jolla, United States
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406 citations
University of Chinese Academy of Sciences
Beijing, China
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138 citations
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JGR · 8 publications · 365 citations
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