The Effect of Stokes Drift and Transient Rip Currents on the Inner Shelf. Part I: No Stratification
The Effect of Stokes Drift and Transient Rip Currents on the Inner Shelf. Part I: No Stratification
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DOI：
10.1175/jpo-d-16-0076.1
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发表时间：
2017-01
影响因子：
3.5
通讯作者：
Nirnimesh Kumar;F. Feddersen
中科院分区：
文献类型：
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作者：
Nirnimesh Kumar;F. Feddersen
AbstractThis是第二部分的两部分的研究重点是斯托克斯漂移和瞬态裂流（TRC）的影响，非分层（第一部分）和分层（本文）内架。第一部分集中在funwaveC耦合海洋大气波浪沉积物传输（COAWST）的耦合和TRC的混合和交换的影响，在一个不分层的内架。在这里，两个模拟（R3和R4）进行分层的内大陆架和surfzone与典型的测深，分层，和波浪条件。R3是仅COAWST模拟（无TRC），而R4具有funwaveC-COAWST耦合（有TRC）。在R4中，TRC导致不规则的近地表冷却、垂直等温线位移和增加的水柱混合。对于R3和R4，平均拉格朗日环流有两个几乎孤立的表面区和内陆架翻转环流圈，以及一个更强的R4内陆架环流圈。R4，内陆架，垂直速度变率是2-3倍强于TRC和无分层的模拟。亲戚...
AbstractThis is Part II of a two-part study focused on Stokes drift and transient rip current (TRC) effects on the unstratified (Part I) and stratified (this paper) inner shelf. Part I focuses on funwaveC–Coupled Ocean–Atmosphere–Wave–Sediment Transport (COAWST) coupling and TRC effects on mixing and exchange on an unstratified inner shelf. Here, two simulations (R3 and R4) are performed on a stratified inner shelf and surfzone with typical bathymetry, stratification, and wave conditions. R3 is a COAWST-only simulation (no TRCs), while R4 has funwaveC–COAWST coupling (with TRCs). In R4, TRCs lead to patchy, near-surface cooling, vertical isotherm displacement, and increased water column mixing. For both R3 and R4, the mean Lagrangian circulation has two nearly isolated surfzones and inner-shelf overturning circulation cells, with a stronger, R4, inner-shelf circulation cell. The R4, inner-shelf, vertical velocity variability is 2–3 times stronger than a simulation with TRCs and no stratification. Relative...