Record Details

Modeling the Lateral Circulation in Straight, Stratified Estuaries*

ScholarsArchive at Oregon State University

Field Value
Title Modeling the Lateral Circulation in Straight, Stratified Estuaries*
Names Lerczak, James A. (creator)
Geyer, W. Rockwell (creator)
Date Issued 2004-06 (iso8601)
Abstract The dynamics of lateral circulation in an idealized, straight estuary under varying stratification conditions is
investigated using a three-dimensional, hydrostatic, primitive equation model in order to determine the importance
of lateral circulation to the momentum budget within the estuary. For all model runs, lateral circulation is about
4 times as strong during flood tides as during ebbs. This flood–ebb asymmetry is due to a feedback between
the lateral circulation and the along-channel tidal currents, as well as to time-varying stratification over a tidal
cycle. As the stratification is increased, the lateral circulation is significantly reduced because of the adverse
pressure gradient set up by isopycnals being tilted by the lateral flow itself. When rotation is included, a timedependent,
cross-channel Ekman circulation is driven, and the tidally averaged, bottom lateral circulation is
enhanced toward the right bank (when looking toward the ocean in the Northern Hemisphere). This asymmetry
in the tidally averaged bottom lateral circulation may lead to asymmetric sediment transport, leading to asymmetric
channel profiles in straight estuaries. For the weakly stratified model run, advection due to lateral currents
is a dominant term in both the along-channel and cross-channel momentum equations over a tidal cycle and for
the tidally averaged momentum equations. In the tidally averaged, along-channel momentum equation, lateral
advection acts as a driving term for the estuarine exchange flow and can be larger than the along-channel pressure
gradient. Therefore, it should not be ignored when estimating momentum budgets in estuaries.
Genre Article
Identifier Lerczak, James A., W. Rockwell Geyer, 2004: Modeling the Lateral Circulation in Straight, Stratified Estuaries*. J. Phys. Oceanogr., 34, 1410–1428.

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