منابع مشابه
Atmospheric forcing of salinity in the overflow of Denmark Strait
Abstract. The temporal evolution of the characteristics of Denmark Strait Overflow Water (DSOW) is reconstructed using hydrographic data and compared with possible atmospheric forcing mechanisms. It is concluded that the main factor influencing the DSOW characteristics at a time scale of one to several years is the difference in mean sea level pressure across Denmark Strait or, in other words, ...
متن کاملThe 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)...
متن کاملVariability 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...
متن کاملSteady Flow Through Modeled Glottal Constriction
The airflow in the modeled glottal constriction was simulated by the solutions of the Navier-Stokes equations for laminar flow, and the corresponding Reynolds equations for turbulent flow in generalized, nonorthogonal coordinates using a numerical method. A two-dimensional model of laryngeal flow is considered and aerodynamic properties are calculated for both laminar and turbulent steady flows...
متن کاملPotential predictability of rapid changes in the Atlantic meridional overturning circulation
[1] We explore the potential predictability of rapid changes in the Atlantic meridional overturning circulation (MOC) using a coupled global climate model (HadCM3). Rapid changes in the temperature and salinity of surface water in the Nordic Seas, and the flow of dense water through Denmark Strait, are found to be precursors to rapid changes in the model’s MOC, with a lead time of around 10 yea...
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ژورنال
عنوان ژورنال: Journal of Geophysical Research: Oceans
سال: 2000
ISSN: 0148-0227
DOI: 10.1029/2000jc900111