Thickness-weighted averaging in tidal estuaries and the vertical distribution of the eulerian residual transport

Knut Klingbeil; Johannes Becherer; Elisabeth Schulz; Huib E. DE SWART; Henk M. Schuttelaars; Arnoldo Valle-Levinson; Hans Burchard

doi:10.1175/JPO-D-18-0083.1

Thickness-weighted averaging in tidal estuaries and the vertical distribution of the eulerian residual transport

Knut Klingbeil^*, Johannes Becherer, Elisabeth Schulz, Huib E. DE SWART, Henk M. Schuttelaars, Arnoldo Valle-Levinson, Hans Burchard

^*Corresponding author for this work

Research output: Contribution to journal › Article › Academic › peer-review

Abstract

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.

Original language	English
Pages (from-to)	1809-1826
Number of pages	18
Journal	Journal of Physical Oceanography
Volume	49
Issue number	7
DOIs	https://doi.org/10.1175/JPO-D-18-0083.1
Publication status	Published - 1 Jul 2019

Keywords

estuaries
baroclinic flows
mass fluxes/transport
tides
filtering techniques
vertical coordinates

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10.1175/JPO-D-18-0083.1

Thickness-Weighted Averaging in Tidal EstuariesFinal published version, 3.95 MBLicence: Taverne

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title = "Thickness-weighted averaging in tidal estuaries and the vertical distribution of the eulerian residual transport",

abstract = "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.",

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author = "Knut Klingbeil and Johannes Becherer and Elisabeth Schulz and {DE SWART}, {Huib E.} and Schuttelaars, {Henk M.} and Arnoldo Valle-Levinson and Hans Burchard",

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doi = "10.1175/JPO-D-18-0083.1",

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T1 - Thickness-weighted averaging in tidal estuaries and the vertical distribution of the eulerian residual transport

AU - Klingbeil, Knut

AU - Becherer, Johannes

AU - Schulz, Elisabeth

AU - DE SWART, Huib E.

AU - Schuttelaars, Henk M.

AU - Valle-Levinson, Arnoldo

AU - Burchard, Hans

PY - 2019/7/1

Y1 - 2019/7/1

N2 - 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.

AB - 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.

KW - estuaries

KW - baroclinic flows

KW - mass fluxes/transport

KW - tides

KW - filtering techniques

KW - vertical coordinates

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U2 - 10.1175/JPO-D-18-0083.1

DO - 10.1175/JPO-D-18-0083.1

M3 - Article

AN - SCOPUS:85066402536

SN - 0022-3670

VL - 49

SP - 1809

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JO - Journal of Physical Oceanography

JF - Journal of Physical Oceanography

IS - 7

ER -

Thickness-weighted averaging in tidal estuaries and the vertical distribution of the eulerian residual transport

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