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Outflows into the Indian Ocean During the Deglaciation Western Pacific, Red Sea, and Pursian Gulf waters flow into the Indian Ocean as surface water outflow at the sill depths ranging from 100 to 300 m.
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Primary outflows · Bab-el-Mandeb, Suez Canal · Basin ... Red Sea's ports and sea routes. ... The Red Sea may be geographically divided into three sections: the Red ...
Sep 10, 2015 · The Red Sea Outflow Water (RSOW), which is formed in the northern Red Sea due to surface buoyancy loss, is one of the most saline water masses ...
The primary aim of this study is to improve the understanding of RSOW formation and its spreading path- ways in the Red Sea. Section 2 introduces the data ...
Saline, dense Red Sea Water (RSW) originates in the northern Red Sea because of an excess of evaporation over precipitation, and enters the Gulf of Aden ( ...
Hydrographic, direct velocity, and subsurface float observations from the 2001 Red Sea Outflow Experi- ment (REDSOX) are analyzed to investigate the ...
The Red Sea outflow exhibits strong seasonal variability in outflow transport due to effects of monsoon winds and seasonal fluctuations in buoyancy forcing.
This south-flowing bottom water, displaced from the north, spills over the sill at Bab el-Mandeb, mostly through the eastern channel. It is estimated that ...
Missing: primary outflows
Feb 19, 2014 · In the southern Red Sea, the low salinity inflow from the Gulf of Aden is intensified along the western boundary due to the beta-effect. In the ...