Climatic Changes in the Dynamic Topography and Geostrophic Circulation of the Arctic Ocean


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Abstract

According to historical oceanographic data, anomalies in the dynamic topography during the winter period were calculated and two climatic stages of dynamic condition of the Arctic Ocean were defined: 1949–1993 and 2007–2013. The associativity of opposition of anomalies in the dynamic topography of the Eurasian and Amerasian basins with fluctuations in the thermal condition of the Northern Atlantic and Pacific oceans, the indexes of atmospheric circulation, river runoff, and change in the area of ice in August of the Laptev, East Siberian, and Chukchi seas is established.

About the authors

L. A. Timokhov

Institute of Arctic and Antarctic Research Institute

Author for correspondence.
Email: ltim@aari.nw.ru
Russian Federation, St. Petersburg

V. V. Ivanov

Institute of Arctic and Antarctic Research Institute; Moscow State University

Email: ltim@aari.nw.ru
Russian Federation, St. Petersburg; Moscow

H. Kassens

GEOMAR Helmholtz Center for Ocean Research

Email: ltim@aari.nw.ru
Germany, Kiel

N. V. Lebedev

Institute of Arctic and Antarctic Research Institute

Email: ltim@aari.nw.ru
Russian Federation, St. Petersburg

I. Ye. Frolov

Institute of Arctic and Antarctic Research Institute

Email: ltim@aari.nw.ru
Russian Federation, St. Petersburg

J. Hölemann

Alfred Wegener Institute

Email: ltim@aari.nw.ru
Germany, Bremerhaven


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