Monthly temperature, salinity, and transport variability of the Bering Strait through flow
نویسندگان
چکیده
منابع مشابه
The Late Quaternary Flow Through the Bering Strait Has Been Forced by the Southern Ocean Winds
Because North and South America are surrounded by water, they constitute together a gigantic island whose peripheral sea level is controlled by the winds east of the island, winds along the western boundary of the island, the freshwater fiux, and the meridional overturning cell. This idea has been expressed in several articles where a series of analytical models show that the Bering Strait (BS)...
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15 صفحه اولVariability of trace-metal fluxes through the Strait of Gibraltar
Van Geen, A. and Boyle, A., 190. Variability of trace-metal fluxes through the Strait of Gibraltar. In: L.D. Labeyrie and C. Jeandel (Editors), Geochemical Variability in the Oceans, Ice and Sediments. Palaeogeogr., Palaeoclimatol., Palaeoecol. (Global Planet. Change Sect.), 89: 65-79.. Three water masses originating in the Atlantic and entering the Alboran Sea through the Strait of Gibraltar h...
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in fact, this study focused on the following questions: 1. is there any difference between the effect of functional/notional approach and the structural approaches to language teaching on the proficiency test of efl learners? 2. can a rather innovative language test referred to as "functional test" ge devised so so to measure the proficiency test of efl learners, and thus be as much reliable an...
15 صفحه اولPliocene cooling enhanced by flow of low-salinity Bering Sea water to the Arctic Ocean
Warming of high northern latitudes in the Pliocene (5.33-2.58 Myr ago) has been linked to the closure of the Central American Seaway and intensification of North Atlantic Deep Water. Subsequent cooling in the late Pliocene may be related to the effects of freshwater input from the Arctic Ocean via the Bering Strait, disrupting North Atlantic Deep Water formation and enhancing sea ice formation....
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ژورنال
عنوان ژورنال: Geophysical Research Letters
سال: 2005
ISSN: 0094-8276
DOI: 10.1029/2004gl021880