Affordable Access

Access to the full text

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

Authors
  • Timokhov, L. A.1
  • Ivanov, V. V.1, 2
  • Kassens, H.3
  • Lebedev, N. V.1
  • Frolov, I. Ye.1
  • Hölemann, J.4
  • 1 Institute of Arctic and Antarctic Research Institute, St. Petersburg, Russia , St. Petersburg (Russia)
  • 2 Moscow State University, Moscow, Russia , Moscow (Russia)
  • 3 GEOMAR Helmholtz Center for Ocean Research, Kiel, Germany , Kiel (Germany)
  • 4 Helmholtz Centre for Polar and Marine Research, Alfred Wegener Institute, Bremerhaven, Germany , Bremerhaven (Germany)
Type
Published Article
Journal
Doklady Earth Sciences
Publisher
Pleiades Publishing
Publication Date
May 01, 2018
Volume
480
Issue
1
Pages
685–688
Identifiers
DOI: 10.1134/S1028334X18050318
Source
Springer Nature
License
Yellow

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.

Report this publication

Statistics

Seen <100 times