Thickness-Weighted Averaging in Tidal Estuaries and the Vertical Distribution of the Eulerian Residual Transport

被引:19
作者
Klingbeil, Knut [1 ,2 ]
Becherer, Johannes [3 ]
Schulz, Elisabeth [2 ]
de Swart, Huib E. [4 ]
Schuttelaars, Henk M. [5 ]
Valle-Levinson, Arnoldo [6 ]
Burchard, Hans [2 ]
机构
[1] Univ Hamburg, Dept Math, Hamburg, Germany
[2] Leibniz Inst Baltic Sea Res Warnemunde IOW, Rostock, Germany
[3] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA
[4] Univ Utrecht, Inst Marine & Atmospher Res Utrecht, Dept Phys, Utrecht, Netherlands
[5] Delft Univ Technol, Delft Inst Appl Math, Delft, Netherlands
[6] Univ Florida, Dept Civil & Coastal Engn, Gainesville, FL USA
关键词
Estuaries; Baroclinic flows; Mass fluxes; transport; Tides; Filtering techniques; Vertical coordinates; CIRCULATION; MODELS; MECHANISMS; FRAMEWORK; VELOCITY; STRESS; BOTTOM; TRACER; WAVES; MASS;
D O I
10.1175/JPO-D-18-0083.1
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
This paper presents thickness-weighted averaging (TWA) in generalized vertical coordinates as a unified framework for a variety of existing tidal-averaging concepts in seas and estuaries. Vertical profiles of resulting residual quantities depend on the specific vertical coordinate, which is held fixed during the averaging process. This dependence is demonstrated through the application to one-dimensional analytical tidal flow with sediment transport, to field observations from a tidal channel, and to model results from a two-dimensional estuary. The use of different coordinate systems provides complementary views on the residual dynamics and stresses the importance of a correct interpretation of residual quantities obtained by tidal averaging.
引用
收藏
页码:1809 / 1826
页数:18
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