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Island Wake in Deep/Shallow Water. Changming Dong James McWilliams Alexander Shchepetkin. IGPP/UCLA. 1. Island Effects in SCB 2. Island Wake in Deep Water 3. Island Wake in Shallow Water. Island Wakes in SCB ( a manuscript to be submitted to CSR). RADARSAT SAR IMAGE
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Island Wake in Deep/Shallow Water Changming Dong James McWilliams Alexander Shchepetkin IGPP/UCLA
1. Island Effects in SCB 2. Island Wake in Deep Water 3. Island Wake in Shallow Water
Island Wakes in SCB ( a manuscript to be submitted to CSR)
RADARSAT SAR IMAGE (Caldeira et al, 2005)
Two Types of Wakes • Deep Water: • the vorticity is generated within lateral boundary • of the island. • 2. Shallow Water: • The vorticty is generated by two ways in homogenous ocean (Signell, 1989): • a. Slope Torque • b. Speed Torque • and additional one with stratification (Smolarkiewicz et al, 1989) • c. Baroclinic tilting
Island Wake in Deep Water (a manuscript submitted to JPO)
An additional nondimensional parameter: Internal Froude Number (Fr), must be introduced in the shallow-water wake.
Summary • In SCB, island wakes is very significant characterizing • SCB circulation. • Three types of instabilities identified in deep-water island • wakes,in which three nondimensional parameters • (Re,Ro and Bu) are dominant. • In the shallow-water wake, an additional dimensionless • parameter (Fr) is important.