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Tidal Front (worked with Drs. H-W. Ou, D. Chen, R. Houghton and M. Visbeck at Lamont, Columbia Univ.)

  (adapted from Dong et al, 2004, JGR)

Due to the inhomogenity in the spatial distribution of tidal mixing, the sea water stratification is homogenized in the shallow water while it is kept in deeper water, thus a tidal front is formed.  Due to seasonal variation in surface heat flux, tidal fronts have two types: winter and summer. A summer tidal front has two branches and a winter tidal front has one. The presence of a tidal front plays an important role in the material and energy tranport in both cross- and along- coast, and affects the local mixing as well. 

Especially, the cross-frontal circulation is one order smaller than the along-frontal flow, however the weak transverse circulation has a significant environmental
implication, such pollution dispersion and nutrient transport.

During my Ph.D study, I studied the cross-frontal circultion applying analytical model, numerical model and dye-tracer field experiment. The analytical solution clearly
shows the cross-frontal circulation is composed of three parts: Ekman flow, Bernoulli circulation and Stokes drift.

References:

 
Current Researches:

  1. Island wakes and their environmental impact.
  2. High-resolution realistic simulation
  3. Southern California Bight Circulation and Forecast System
  4. Bering Sea Ice-Ecological-coupled System
  5. Sediment Transport
  6. Pollution (such as DDTs) Dispersion and Water Quality Assessment

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