Effects of atmospheric vorticity on the seasonal hydrographic cycle over the eastern Siberian shelf

Physics

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Oceanography: General: Arctic And Antarctic Oceanography (9310, 9315), Oceanography: General: Diurnal, Seasonal, And Annual Cycles (0438), Oceanography: General: Climate And Interannual Variability (1616, 1635, 3305, 3309, 4513), Oceanography: General: Continental Shelf And Slope Processes (3002), Oceanography: Physical: Air/Sea Interactions (0312, 3339)

Scientific paper

The seasonal hydrographic cycle explains about 25-75% of the entire salinity variability spectrum of the Siberian shelf hydrography. Quasi-decadal variations in the seasonal salinity difference over the Laptev and East Siberian sea shelves derived from continuous summer-to-winter historical records from the 1960s-1990s are attributed to atmospheric vorticity quasi-decadal variations. Summer cyclonic vorticity results in riverine water accumulation on the shelf, increasing the salinity summer-to-winter difference. Summer anticyclonic wind pattern enhances fresh water movement from the shelf towards the Arctic Ocean that tends to weaken the seasonal salinity amplitude.

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