Physics
Scientific paper
Jul 2009
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009georl..3613605d&link_type=abstract
Geophysical Research Letters, Volume 36, Issue 13, CiteID L13605
Physics
6
Oceanography: General: Arctic And Antarctic Oceanography (9310, 9315), Oceanography: General: Continental Shelf And Slope Processes (3002), Oceanography: Physical: Decadal Ocean Variability (1616, 1635, 3305, 4215), Oceanography: Physical: Ice Mechanics And Air/Sea/Ice Exchange Processes (0700, 0750, 0752, 0754), Cryosphere: Sea Ice (4540)
Scientific paper
The winter net sea-ice production (NSIP) over the Laptev Sea shelf is inferred from continuous summer-to-winter historical salinity records of 1960s-1990s. While the NSIP strongly depends on the assumed salinity of newly formed ice, the NSIP quasi-decadal variability can be linked to the wind-driven circulation anomalies in the Laptev Sea region. The increased wind-driven advection of ice away from the Laptev Sea coast when the Arctic Oscillation (AO) is positive implies enhanced coastal polynya sea-ice production and brine release in the shelf water. When the AO is negative, the NSIP and seasonal salinity amplitude tends to weaken. These results are in reasonable agreement with sea-ice observations and modeling.
Bauch Dorothea
Dmitrenko Igor A.
Kirillov Sergey A.
Tremblay L.-Bruno
Willmes Sascha
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