ON REPRESENTATION OF REYNOLDS STRESS IN A TIDAL ESTUARY

被引：10

作者：

JOHNS, B

机构：

[1] Department of Geography, The University Reading, Reading

来源：

GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY | 1969年 / 17卷 / 01期

关键词：

D O I：

10.1111/j.1365-246X.1969.tb06377.x

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

The parametric representation of turbulence by a coefficient of eddy viscosity is discussed for the tidal flow in a river estuary. If the eddy viscosity attains a specified maximum value in the mid‐depths, it is shown that the amplitude of the tidal current has a logarithmic profile throughout the depth. Copyright © 1969, Wiley Blackwell. All rights reserved

引用

页码：39 / &

共 4 条

[1] THE DISTRIBUTION OF SHEARING STRESSES IN A TIDAL CURRENT [J].

BOWDEN, KF ;

FAIRBAIRN, LA ;

HUGHES, P .

GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1959, 2 (04) :288-305

[2] ON VERTICAL STRUCTURE OF TIDAL FLOW IN RIVER ESTUARIES [J].

JOHNS, B ;

ODD, N .

GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1966, 12 (01) :103-&

[3] SOME EFFECTS OF TOPOGRAPHY ON TIDAL FLOW IN A RIVER ESTUARY [J].

JOHNS, B .

GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1968, 15 (05) :501-&

[4] TIDAL FLOW AND MASS TRANSPORT IN A SLOWLY CONVERGING ESTUARY [J].

JOHNS, B .

GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1967, 13 (04) :377-&

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