TENSOR STRESS ASYMMETRY AS A MECHANISM FOR THE FORMATION OF DIPOLE VORTEX INTO THE JET FLOW IN THE COASTAL ZONE

A. V. Dan'shina; V. Chancev

doi:10.31519/conferencearticle_5b5ce399cb5f22.68516349

Home / Conferences / XXIV International Coastal Conference "SEA COASTS – EVOLUTION, ECOLOGY, ECONOMY"

CSCSTI 06.01 BISAC NAT010000 BISAC NAT045050 BISAC NAT025000 BISAC NAT045030 BISAC SCI081000 BISAC SCI092000 BISAC SCI020000 BISAC SCI039000 BISAC SOC053000 BISAC TEC060000

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TENSOR STRESS ASYMMETRY AS A MECHANISM FOR THE FORMATION OF DIPOLE VORTEX INTO THE JET FLOW IN THE COASTAL ZONE

Section: HYDRO-, MORPHOAND LITHODYNAMICS OF SEA COASTS AND ADJACENT WATERS

Type:

Conference article

DOI:

https://doi.org/10.31519/conferencearticle_5b5ce399cb5f22.68516349

Pages:

121–122

Language:

Russian, English

A. V. Dan'shina ¹

V. Chancev ²

A. V. Dan'shina

Rossiyskiy gosudarstvennyy gidrometeorologicheskiy universitet (RGGMU)

V. Chancev

Rossiyskiy gosudarstvennyy gidrometeorologicheskiy universitet (RGGMU)

Russian Federation

Abstract:
The theoretical conclusions about the effect of asymmetry of the stress tensor on the formation of dipolar vortex structures are built on the basis of laboratory experiments. The results of computer simulation of the mushroom current are provided.

Keywords:
the theoretical

Грибовидные течения в океане являются универсальной формой движения вод и играют важную роль в горизонтальном обмене примесями, массой и количеством движения. Таким образом, их влияние сказывается на формировании гидродинамического режима и экологической обстановки в море в целом и особенно в его прибрежных районах. Такие структуры выявляются как на спутниковых изображениях поверхности океанов и морей, так и в результате анализа прямых натурных наблюдений за термодинамическими параметрами верхних слоев океана.

1. net spiska literatury

GOST

Dan'shina A. V., Chancev V. Y. TENSOR STRESS ASYMMETRY AS A MECHANISM FOR THE FORMATION OF DIPOLE VORTEX INTO THE JET FLOW IN THE COASTAL ZONE // XXIV International Coastal Conference "SEA COASTS – EVOLUTION, ECOLOGY, ECONOMY". 2012. pp. 121-122. DOI: https://doi.org/10.31519/conferencearticle_5b5ce399cb5f22.68516349. (Date of access 02.11.2026).

MLA

A. V. Dan'shina, Chancev V. Y.. "TENSOR STRESS ASYMMETRY AS A MECHANISM FOR THE FORMATION OF DIPOLE VORTEX INTO THE JET FLOW IN THE COASTAL ZONE." XXIV International Coastal Conference "SEA COASTS – EVOLUTION, ECOLOGY, ECONOMY" (2012): 121-122. DOI: https://doi.org/10.31519/conferencearticle_5b5ce399cb5f22.68516349.

APA

Dan'shina A. V., Chancev V. Y. (2012). TENSOR STRESS ASYMMETRY AS A MECHANISM FOR THE FORMATION OF DIPOLE VORTEX INTO THE JET FLOW IN THE COASTAL ZONE. XXIV International Coastal Conference "SEA COASTS – EVOLUTION, ECOLOGY, ECONOMY", 121-122. https://doi.org/10.31519/conferencearticle_5b5ce399cb5f22.68516349

Chicago

A. V. Dan'shina, Chancev V. Y.. "TENSOR STRESS ASYMMETRY AS A MECHANISM FOR THE FORMATION OF DIPOLE VORTEX INTO THE JET FLOW IN THE COASTAL ZONE." XXIV International Coastal Conference "SEA COASTS – EVOLUTION, ECOLOGY, ECONOMY", no. (2012): 121-122. https://doi.org/10.31519/conferencearticle_5b5ce399cb5f22.68516349.

WIKI

{{cite journal | author = Dan'shina A. V., Chancev V. Y. | title = TENSOR STRESS ASYMMETRY AS A MECHANISM FOR THE FORMATION OF DIPOLE VORTEX INTO THE JET FLOW IN THE COASTAL ZONE | journal = XXIV International Coastal Conference "SEA COASTS – EVOLUTION, ECOLOGY, ECONOMY" | year = 2012 | pages = 121-122 | doi = 10.31519/conferencearticle_5b5ce399cb5f22.68516349 }}

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