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Global Atmospheric Circulation Patterns and Relationships to Arctic Freshwater Fluxes

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The Freshwater Budget of the Arctic Ocean

Part of the book series: NATO Science Series ((ASEN2,volume 70))

Abstract

The large-scale atmospheric circulation affects the Arctic Ocean’s freshwater fluxes in at least three ways. First, the circulation controls the direct fluxes of precipitation (P) and evaporation (E) at the Arctic Ocean’s surface through the pattern of atmospheric moisture inflow and its convergence over the Arctic Ocean. Second, the circulation determines P and E over the Arctic terrestrial watersheds; the net P-E eventually reaches the Arctic Ocean as river runoff. Third, the large-scale circulation provides the wind-forcing that drives the advective fluxes of sea ice and ocean freshwater anomalies into and out of the Arctic (e.g., through Bering and Fram Straits) as well as from one portion of the Arctic Ocean to another. The atmospheric thermal anomalies resulting from the large-scale circulation also modify the freshwater fluxes in the Arctic Ocean through the freezing and melting of sea ice. This thermodynamic forcing is often correlated with the wind-driven forcing on interannual timescales.

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© 2000 Springer Science+Business Media Dordrecht

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Walsh, J.E. (2000). Global Atmospheric Circulation Patterns and Relationships to Arctic Freshwater Fluxes. In: Lewis, E.L., Jones, E.P., Lemke, P., Prowse, T.D., Wadhams, P. (eds) The Freshwater Budget of the Arctic Ocean. NATO Science Series, vol 70. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-4132-1_2

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  • DOI: https://doi.org/10.1007/978-94-011-4132-1_2

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-0-7923-6440-5

  • Online ISBN: 978-94-011-4132-1

  • eBook Packages: Springer Book Archive

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