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The General Circulation in a Dissipative Ocean Basin with Longshore Wind Stresses
Dissipative Ocean Basin Longshore Wind Stresses western boundary current
2009/2/6
Solutions of the Stommel equation are presented which take the form of free waves in the interior of the ocean basin, driven by convergences and divergences in coastal transports brought about by the ...
A Two-Level Model of a Thermally Forced Ocean Basin
Two-Level Model Thermally Forced Ocean Basin
2009/1/22
Some simple solutions (mostly analytic) are presented for the large-scale baroclinic response to thermal forcing on a mid-latitude beta-plane. Surface heat flux is parameterized as (TA–TT)/tau;, with ...
Buoyancy-Driven Circulation in an Ocean Basin with Isopycnals Intersecting the Sloping Boundary
potential vorticity Buoyancy-Driven Circulation Ocean Basin Sloping Boundary
2008/12/10
The dynamics that govern the spreading of a convectively formed water mass in an ocean with sloping boundaries are examined using an isopycnal model that permits the interface between the layers to in...
The roles of ENSO on the occurrence of abruptly recurving tropical cyclones over the Western North Pacific Ocean Basin
ENSO recurving tropical cyclones the Western North Pacific Ocean Basin
2010/1/25
The abruptly recurving tropical cyclones over the Western North Pacific Ocean Basin during El Niño and La Niña events are studied. Temporal and spatial variations of these anomalous trac...