作者: Jianrong Zhu , Changsheng Chen , Elise Ralph , Sarah A. Green , Judith Wells Budd
DOI: 10.1175/1520-0485(2001)031<0396:PMSOTK>2.0.CO;2
关键词: Current (stream) 、 Wind forcing 、 Heat flux 、 Buoy 、 Peninsula 、 Geology 、 Submarine pipeline 、 Heat transfer 、 Atmospheric sciences 、 Meteorology 、 Forcing (mathematics)
摘要: The Keweenaw Current, observed along the coast of Peninsula in Lake Superior during July 1973, was simulated using a 3D, nonorthogonal coordinate transformation, primitive equation coastal ocean model. model domain covered entire lake with high resolution 250‐600 m cross-shelf direction and 4‐6 km alongshelf peninsula. initialized monthly averaged temperature field June 1973 run prognostically synoptic wind forcing plus heat flux. Good agreement found between model-predicted currents at buoy stations near Eagle Harbor. Comparison results without inclusion flux suggested that combined fluxes played key role intensification Current summer months. relatively strong near-inertial oscillations occurred episodically under conditions clockwise-rotating wind. These intensified surface, were weak coast, increased significantly offshore.