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SVERDRUP TRANSPORT IN THE NORTH ATLANTIC

Abstract

Monthly values of the latitudinal mass transport in the North Atlanticbased on the Sverdrup relation are analyzed. A continuous wind stress dataset NOC v 1.1 with a spatial resolution of 1×1° for the period of 1980—2005 is used as a basic data. Estimates of the Sverdrup transport values in the area of subtropical gyre showed the maximum of mean annual Sverdrup transport values (−29,8×106 m3/s) on 33 °N. The quasi-latitudinal (zonal) barotropic wind transport values were calculated as a summation of maximum Sverdrup transport values in subtropical and subpolar gyres, and their seasonal and interannual variability was examined. The correlation analysis of the annual values of zonal transport and NAO index indicates a significant inverse correlation (r = −0,6), which confirms the Bjerknes’ compensation theory suggesting that transports in the ocean and the atmosphere covariate in an out-ofphase manner in theNorth Atlantic region. 

About the Authors

S. A. Dobrolyubov
Lomonosov Moscow State University
Russian Federation


E. I. Klimchuk
Lomonosov Moscow State University
Russian Federation


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Review

For citations:


Dobrolyubov S.A., Klimchuk E.I. SVERDRUP TRANSPORT IN THE NORTH ATLANTIC. Vestnik Moskovskogo universiteta. Seriya 5, Geografiya. 2014;(2):25-31. (In Russ.)

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ISSN 0579-9414 (Print)