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Wintertime Interactions of the Atmosphere with the Mediterranean Sea
Wintertime Interactions Mediterranean Sea Atmosphere
2009/4/3
The net loss of heat by the Mediterranean Sea was determined for February 1969 while oceanographers observed the cooling and sinking of the water south of France. The heat loss during the four precedi...
Wintertime Winds and Coastal Sea-Level Fluctuations in the Northeast China Sea. Part I：Observations
Wintertime Winds Northeast China Sea Coastal Sea-Level Fluctuations
2009/2/6
Analyses of low-pass filtered coastal sea-level data and geostrophic winds derived from surface pressure charts for the period of 1 December 1980 through 31 March 1981 indicate that the wintertime dyn...
Wintertime Convection in a Gulf stream Warm Core Ring
Wintertime Convection Gulf stream Warm Core Ring
2009/1/16
Wintertime convection creates deep mixed layers which determine the water mass characteristics and potential vorticity for waters in the main pycnocline of the world ocean. Diabatic cooling is most in...
Wintertime Winds and Coastal Sea-Level Fluctuations in the Northeast China Sea. Part II：Numerical Model
Wintertime Winds Northeast China Sea Coastal Sea-Level Fluctuations Numerical Model
2009/1/10
As a sequel to data analysis reported in Part I, a numerical model of the wintertime wind-driven circulation of the northeast Chine Sea is developed with the primary purpose of achieving an understand...
A Mechanism for the Recurrence of Wintertime Midlatitude SST Anomalies
ocean temperature deep mixed layer Wintertime Midlatitude
2008/12/11
In the early 1970s, Namias and Born speculated that ocean temperature anomalies created over the deep mixed layer in winter could be preserved in the summer thermocline and reappear at the surface in ...
Interannual Variability of the Kuroshio Extension System and Its Impact on the Wintertime SST Field
Interannual Variability Kuroshio Extension System Wintertime SST Field
2008/6/30
Altimetry data from the first 7-yr TOPEX/Poseidon (T/P) mission (October 1992–September 1999) are analyzed to investigate the interannual variability in regions of the Kuroshio Extension and its south...
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...