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The role of sea ice and other fresh water in the Arctic circulation
Salinity stratification is critical to the vertical circulation of the high-latitude ocean. We here examine the control of the vertical circulation in the northern seas, and the potential for…
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Direct measurements of transport and water properties through the Bering Strait
Four years of temperature, salinity, and velocity data enable a direct computation of volume transport and a temporal description of water properties exchanged through the Bering Strait. The mean…
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Revising the Bering Strait freshwater flux into the Arctic Ocean
The freshwater flux through the Bering Strait into the Arctic Ocean is important regionally and globally, e.g. for Chukchi Sea hydrography, Arctic Ocean stratification, the global freshwater cycle,…
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Thermohaline circulation in the Arctic Mediterranean Seas
The renewal of the deep North Atlantic by the various overflows of the Greenland-Scotland ridges is only one manifestation of the convective and mixing processes which occur in the various basins and…
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The large‐scale freshwater cycle of the Arctic
This paper synthesizes our understanding of the Arctic's large-scale freshwater cycle. It combines terrestrial and oceanic observations with insights gained from the ERA-40 reanalysis and land…
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On the halocline of the Arctic Ocean
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Monthly temperature, salinity, and transport variability of the Bering Strait through flow
The Bering Strait through flow is important for the Chukchi Sea and the Arctic and Atlantic oceans. A realistic assessment of through flow properties is also necessary for validation and boundary…
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Bering Strait the Regional Physical Oceanography
Find loads of the bering strait the regional physical oceanography book catalogues in this site as the choice of you visiting this page. You can also join to the website book library that will show…
A year in the physical oceanography of the Chukchi Sea: Moored measurements from autumn 1990–1991
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Transports through Bering Strait: Annual and interannual variability
Reanalysis of the 1976–1977 mean monthly transport estimates for Bering Strait of Coachman and Aagaard (1981) shows a considerably stronger wind dependence than was calculated by Aagaard et al.…
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