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THE INTERACTION BETWEEN ESTUARINE PL...
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ProQuest Information and Learning Co.
THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).
Record Type:
Language materials, manuscript : Monograph/item
Title/Author:
THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA)./
Author:
ZHANG, QINGHUA.
Description:
1 online resource (79 pages)
Notes:
Source: Dissertation Abstracts International, Volume: 47-01, Section: B, page: 1200.
Subject:
Physical oceanography. -
Online resource:
click for full text (PQDT)
THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).
ZHANG, QINGHUA.
THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).
- 1 online resource (79 pages)
Source: Dissertation Abstracts International, Volume: 47-01, Section: B, page: 1200.
Thesis (Ph.D.)--North Carolina State University, 1985.
Includes bibliographical references
A simple analytical model is developed to describe the steady flow in an estuary-shelf interaction region where the water is treated as a two-layer density stratified flow. The motion is expanded in terms of the relative thickness of the Ekman layer, E(,v)(' 1/2). The order-zero flow is geostrophic in each layer. Balancing of order-one quantities reduces the system to two vorticity equations relating the pressure field with the displacement of the interface and the bottom topography. An explicit solution is obtained for the case of linear offshore sloping bottom. The flow behaviour of the river water plume depends on the vertical structure of the flow at the river mouth, the bottom topography and the ambient coastal flow. Under certain conditions, a salinity front exists as an offshore boundary of the river plume. These results are compared with observations for the Changjiang River (in China), and the Chesapeake Bay and Savannah River (in US) estuaries.
Electronic reproduction.
Ann Arbor, Mich. :
ProQuest,
2018
Mode of access: World Wide Web
Subjects--Topical Terms:
1178843
Physical oceanography.
Index Terms--Genre/Form:
554714
Electronic books.
THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).
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THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).
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Source: Dissertation Abstracts International, Volume: 47-01, Section: B, page: 1200.
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Thesis (Ph.D.)--North Carolina State University, 1985.
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Includes bibliographical references
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A simple analytical model is developed to describe the steady flow in an estuary-shelf interaction region where the water is treated as a two-layer density stratified flow. The motion is expanded in terms of the relative thickness of the Ekman layer, E(,v)(' 1/2). The order-zero flow is geostrophic in each layer. Balancing of order-one quantities reduces the system to two vorticity equations relating the pressure field with the displacement of the interface and the bottom topography. An explicit solution is obtained for the case of linear offshore sloping bottom. The flow behaviour of the river water plume depends on the vertical structure of the flow at the river mouth, the bottom topography and the ambient coastal flow. Under certain conditions, a salinity front exists as an offshore boundary of the river plume. These results are compared with observations for the Changjiang River (in China), and the Chesapeake Bay and Savannah River (in US) estuaries.
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Ann Arbor, Mich. :
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ProQuest,
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2018
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Mode of access: World Wide Web
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Physical oceanography.
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click for full text (PQDT)
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