The large-scale freshwater cycle of the Arctic
Serreze, Mark C.; Barrett, Andrew P.; Slater, Andrew G.; Woodgate, Rebecca A.; Aagaard, Knut; Lammers, Richard B.; Steele, Michael; Moritz, Richard; Meredith, Michael ORCID: https://orcid.org/0000-0002-7342-7756; Lee, Craig M.. 2006 The large-scale freshwater cycle of the Arctic. Journal of Geophysical Research, 111 (C11), C11010. 19, pp. https://doi.org/10.1029/2005JC003424
Full text not available from this repository. (Request a copy)Abstract/Summary
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 surface and ice-ocean models. Annual mean freshwater input to the Arctic Ocean is dominated by river discharge (38%), inflow through Bering Strait (30%), and net precipitation (24%). Total freshwater export from the Arctic Ocean to the North Atlantic is dominated by transports through the Canadian Arctic Archipelago (35%) and via Fram Strait as liquid (26%) and sea ice (25%). All terms are computed relative to a reference salinity of 34.8. Compared to earlier estimates, our budget features larger import of freshwater through Bering Strait and larger liquid phase export through Fram Strait. While there is no reason to expect a steady state, error analysis indicates that the difference between annual mean oceanic inflows and outflows (∼8% of the total inflow) is indistinguishable from zero. Freshwater in the Arctic Ocean has a mean residence time of about a decade. This is understood in that annual freshwater input, while large (∼8500 km3), is an order of magnitude smaller than oceanic freshwater storage of ∼84,000 km3. Freshwater in the atmosphere, as water vapor, has a residence time of about a week. Seasonality in Arctic Ocean freshwater storage is nevertheless highly uncertain, reflecting both sparse hydrographic data and insufficient information on sea ice volume. Uncertainties mask seasonal storage changes forced by freshwater fluxes. Of flux terms with sufficient data for analysis, Fram Strait ice outflow shows the largest interannual variability.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | https://doi.org/10.1029/2005JC003424 |
Programmes: | BAS Programmes > Other Special Projects |
ISSN: | 0148-0227 |
Additional Information. Not used in RCUK Gateway to Research.: | Full text not available from this repository |
Additional Keywords: | Hydrology, Oceanography |
NORA Subject Terms: | Marine Sciences Hydrology |
Date made live: | 11 Sep 2007 14:22 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/971 |
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