Sea-Breeze Modification Of The Growth Of A Marine Internal Boundary Layer

摘要: A numerical mesoscale model is used to make a high-resolution simulation of the marine boundary layer in Persian Gulf, during conditions offshore flow from Saudi Arabia. internal (MIBL) and sea-breeze circulation (SBC) are found co-exist. The sea breeze develops mid-afternoon, at which time its front displaced several tens kilometres offshore. Between coast system, MIBL that occurs consistent with picture described existing literature. However, perturbed by SBC, deepening significantly seaward front. Our analysis suggests this strong, localized not direct consequence frontal uplift, but rather immediate cause retardation prevailing, low-level wind SBC. simulated boundary-layer development can be accounted for using simple 1D Lagrangian growth driven surface heat flux. This obtained as straightforward modification an established analytic model.