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Nongeostrophic Baroclinic Instability over Sloping Bathymetry: Buoyant Flow Regime

Nongeostrophic Baroclinic Instability over Sloping Bathymetry: Buoyant Flow Regime

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2492021513

Nongeostrophic Baroclinic Instability over Sloping Bathymetry: Buoyant Flow Regime

About this item

Full title

Nongeostrophic Baroclinic Instability over Sloping Bathymetry: Buoyant Flow Regime

Author / Creator

Publisher

Boston: American Meteorological Society

Journal title

Journal of physical oceanography, 2020-07, Vol.50 (7), p.1937-1956

Language

English

Formats

Publication information

Publisher

Boston: American Meteorological Society

More information

Scope and Contents

Contents

Baroclinic instabilities are important processes that enhance mixing and dispersion in the ocean. The presence of sloping bathymetry and the nongeostrophic effect influence the formation and evolution of baroclinic instabilities in oceanic bottom boundary layers and in coastal waters. This study explores two nongeostrophic baroclinic instability th...

Alternative Titles

Full title

Nongeostrophic Baroclinic Instability over Sloping Bathymetry: Buoyant Flow Regime

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2492021513

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2492021513

Other Identifiers

ISSN

0022-3670

E-ISSN

1520-0485

DOI

10.1175/JPO-D-19-0145.1

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