The marine hydrological cycle: The ocean's floods and droughts

Abstract The sea surface salinity (SSS) displays fluctuations that are not solely in response to local air‐sea flux of freshwater but also reflect ocean circulation and mixing processes. Ponte and Vinogradova (2016), using Estimating the Circulation and Climate of the Ocean output, estimate the rela...

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Bibliographic Details
Main Author: Arnold L. Gordon
Format: Article
Language:English
Published: Wiley 2016-07-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1002/2016GL070279
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Summary:Abstract The sea surface salinity (SSS) displays fluctuations that are not solely in response to local air‐sea flux of freshwater but also reflect ocean circulation and mixing processes. Ponte and Vinogradova (2016), using Estimating the Circulation and Climate of the Ocean output, estimate the relative roles of these forces for the global ocean. They find that the governing forces vary greatly across ocean regimes. Their research identifies features that will be addressed with enhanced SSS observations from orbiting satellites and in situ global arrays, which promise new insight into the marine water cycle and its place in the global hydrological system.
ISSN:0094-8276
1944-8007