A link between winter precipitation in Europe and the Arctic Sea ice, sea surface temperature, and atmospheric circulation


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

The spatial and temporal pattern of the link between the winter precipitation variability and variations in the North Atlantic sea surface temperature, the Arctic sea ice concentration, and 500 hPa geopotential height in the Northern Hemisphere is analyzed for the period of 1952-2012. The analysis reveals two principal modes of covariability in the analyzed characteristics. The first mode which explains the most part of covariability, is related to the impact of the North Atlantic Oscillation. The second mode indicates the significant contribution of the Atlantic Multidecadal Oscillation associated with winter precipitation anomalies of the same sign in Europe with the maxima on the East European Plain and in the Balkan region during the positive phase of AMO.

作者简介

E. Cherenkova

Institute of Geography

编辑信件的主要联系方式.
Email: cherenkova@igras.ru
俄罗斯联邦, Staromonetnyiper. 29, Moscow, 119017

V. Semenov

Institute of Geography; Obukhov Institute of Atmospheric Physics

Email: cherenkova@igras.ru
俄罗斯联邦, Staromonetnyiper. 29, Moscow, 119017; Pyzhevskii per. 3, Moscow, 119017

补充文件

附件文件
动作
1. JATS XML

版权所有 © Allerton Press, Inc., 2017