TOPOLOGICAL PHASE TRANSITIONS IV: DYNAMIC THEORY OF BOUNDARY-LAYER SEPARATIONS

We present in this paper a systematic dynamic theory for boundary-layer separations of fluid flows and its applications to large scale ocean circulations, based on the geometric theory of incompressible flows developed by the authors. First, we derive the separation equations, which provide necessar...

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Main Authors: Ma, Tian, Wang, Shouhong
Other Authors: Sichuan University Chengdu (SCU), Indiana University Bloomington, Indiana University System
Format: Report
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-01672759
https://hal.archives-ouvertes.fr/hal-01672759/document
https://hal.archives-ouvertes.fr/hal-01672759/file/tpt4.pdf
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spelling ftccsdartic:oai:HAL:hal-01672759v1 2023-05-15T17:32:24+02:00 TOPOLOGICAL PHASE TRANSITIONS IV: DYNAMIC THEORY OF BOUNDARY-LAYER SEPARATIONS Ma, Tian Wang, Shouhong Sichuan University Chengdu (SCU) Indiana University Bloomington Indiana University System 2017-12-27 https://hal.archives-ouvertes.fr/hal-01672759 https://hal.archives-ouvertes.fr/hal-01672759/document https://hal.archives-ouvertes.fr/hal-01672759/file/tpt4.pdf en eng HAL CCSD hal-01672759 https://hal.archives-ouvertes.fr/hal-01672759 https://hal.archives-ouvertes.fr/hal-01672759/document https://hal.archives-ouvertes.fr/hal-01672759/file/tpt4.pdf info:eu-repo/semantics/OpenAccess https://hal.archives-ouvertes.fr/hal-01672759 2017 [NLIN.NLIN-PS]Nonlinear Sciences [physics]/Pattern Formation and Solitons [nlin.PS] [PHYS.MPHY]Physics [physics]/Mathematical Physics [math-ph] info:eu-repo/semantics/preprint Preprints, Working Papers, . 2017 ftccsdartic 2020-12-25T06:55:37Z We present in this paper a systematic dynamic theory for boundary-layer separations of fluid flows and its applications to large scale ocean circulations, based on the geometric theory of incompressible flows developed by the authors. First, we derive the separation equations, which provide necessary and sufficient conditions for the flow separation at a boundary point. Second, these separation equations are then further converted to predicable conditions, which can be used to determine precisely when, where, and how a boundary-layer separation occurs. Third, we derive conditions for the formation of vortices from boundary tip points, and conditions for the formation of surface turbulence. Fourth, we derive the mechanism of the formation of the subpolar gyre and the formation of the small scale wind-driven vortex oceanic flows, in the north Atlantic ocean. Report North Atlantic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Boundary Point ENVELOPE(-98.266,-98.266,59.970,59.970)
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [NLIN.NLIN-PS]Nonlinear Sciences [physics]/Pattern Formation and Solitons [nlin.PS]
[PHYS.MPHY]Physics [physics]/Mathematical Physics [math-ph]
spellingShingle [NLIN.NLIN-PS]Nonlinear Sciences [physics]/Pattern Formation and Solitons [nlin.PS]
[PHYS.MPHY]Physics [physics]/Mathematical Physics [math-ph]
Ma, Tian
Wang, Shouhong
TOPOLOGICAL PHASE TRANSITIONS IV: DYNAMIC THEORY OF BOUNDARY-LAYER SEPARATIONS
topic_facet [NLIN.NLIN-PS]Nonlinear Sciences [physics]/Pattern Formation and Solitons [nlin.PS]
[PHYS.MPHY]Physics [physics]/Mathematical Physics [math-ph]
description We present in this paper a systematic dynamic theory for boundary-layer separations of fluid flows and its applications to large scale ocean circulations, based on the geometric theory of incompressible flows developed by the authors. First, we derive the separation equations, which provide necessary and sufficient conditions for the flow separation at a boundary point. Second, these separation equations are then further converted to predicable conditions, which can be used to determine precisely when, where, and how a boundary-layer separation occurs. Third, we derive conditions for the formation of vortices from boundary tip points, and conditions for the formation of surface turbulence. Fourth, we derive the mechanism of the formation of the subpolar gyre and the formation of the small scale wind-driven vortex oceanic flows, in the north Atlantic ocean.
author2 Sichuan University Chengdu (SCU)
Indiana University Bloomington
Indiana University System
format Report
author Ma, Tian
Wang, Shouhong
author_facet Ma, Tian
Wang, Shouhong
author_sort Ma, Tian
title TOPOLOGICAL PHASE TRANSITIONS IV: DYNAMIC THEORY OF BOUNDARY-LAYER SEPARATIONS
title_short TOPOLOGICAL PHASE TRANSITIONS IV: DYNAMIC THEORY OF BOUNDARY-LAYER SEPARATIONS
title_full TOPOLOGICAL PHASE TRANSITIONS IV: DYNAMIC THEORY OF BOUNDARY-LAYER SEPARATIONS
title_fullStr TOPOLOGICAL PHASE TRANSITIONS IV: DYNAMIC THEORY OF BOUNDARY-LAYER SEPARATIONS
title_full_unstemmed TOPOLOGICAL PHASE TRANSITIONS IV: DYNAMIC THEORY OF BOUNDARY-LAYER SEPARATIONS
title_sort topological phase transitions iv: dynamic theory of boundary-layer separations
publisher HAL CCSD
publishDate 2017
url https://hal.archives-ouvertes.fr/hal-01672759
https://hal.archives-ouvertes.fr/hal-01672759/document
https://hal.archives-ouvertes.fr/hal-01672759/file/tpt4.pdf
long_lat ENVELOPE(-98.266,-98.266,59.970,59.970)
geographic Boundary Point
geographic_facet Boundary Point
genre North Atlantic
genre_facet North Atlantic
op_source https://hal.archives-ouvertes.fr/hal-01672759
2017
op_relation hal-01672759
https://hal.archives-ouvertes.fr/hal-01672759
https://hal.archives-ouvertes.fr/hal-01672759/document
https://hal.archives-ouvertes.fr/hal-01672759/file/tpt4.pdf
op_rights info:eu-repo/semantics/OpenAccess
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