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Negative Oceanic Heat Flux as a Cause of Water-Mass Formation
Negative Oceanic Heat Flux Water-Mass Formation
2009/4/3
Regions of large (>60 kcal cm−2 year−1) net annual heat flux from the oceans to the atmosphere are found only on the western sides of Northern Hemisphere oceans and in the Norwegian Sea, a...
Winter Circulation in the Western Gulf of Maine：Part 1. Cooling and Water Mass Formation
Winter Circulation Western Gulf Water Mass Formation
2009/2/23
The mean circulation on the northeast continental shelf in the region of the Gulf of Mexico is discussed in terms of a simple box model, based on volume transports and mean salinities estimated from e...
Mixing and Water-Mass Formation in the Australian Subantarctic
Water-Mass Formation Australian Subantarctic
2009/2/10
A cruise south of eastern Australia confirmed the formation of a Subantarctic Mode Water type in late winter on the equatorward side of the Subantarctic Front. This water type, mixed with the winter s...
Poleward heat transport by the own implies warm Water mass formation, i.e., the retention by the tropical and subtropical ocean of some of its net radiant heat gain. Under what condition net heat rete...
The Relationship between Water Mass Formation and the Surface Buoyancy Flux, with Application to Phillips’ Red Sea Model
Water Mass Formation Surface Buoyancy Flux Red Sea Model
2008/12/12
A buoyancy flux across the sea surface between the outcropping of isopycnals must be balanced by a subsurface diapycnal buoyancy flux. If this flux were only advective, its derivative with respect to ...
Antarctic Intermediate Water Mass Formation in Ocean General Circulation Models
Antarctic Intermediate Water Mass Formation Ocean General Circulation Models
2008/7/25
Antarctic Intermediate Water is formed at the high midlatitudes of the Southern Ocean. In many ocean general circulation model simulations with coarse resolution and a z coordinate, a middepth salinit...
Diagnosing Water Mass Formation from Air–Sea Fluxes and Surface Mixing
Diagnosing Water Mass Air–Sea Fluxes Surface Mixing
2008/7/16
The formation rate of water masses and its relation to air–sea fluxes and interior mixing are examined in an isopycnic model of the North (and tropical) Atlantic that includes a mixed layer. The diagn...
The Wintertime Water Mass Formation in the Northern Arabian Sea: A Model Study
Water Mass Formation Northern Arabian Sea
2008/6/4
Using a level 2 one-dimensional turbulent closure model, the evolution of the Arabian Sea High Salinity Water mass (ASHSW) has been studied. Model-derived heat fluxes, sea surface temperature (SST), a...
