A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2022; you can also visit the original URL.
The file type is
The influence of autumn Eurasian snow cover on the atmospheric dynamics anomalies during the following winter is studied based on the INM RAS climate model data. The North Atlantic Oscillation is the leading pattern that causes the weather and climate variability in the Northern hemisphere. We evaluate the up-to-date model version (INMCM5) ability of the autumn Eurasian snow -winter NAO teleconnection simulation on different timescales. Maximum covariance analysis (MCA) is used to find winterdoi:10.14529/jsfi210403 dblp:journals/superfri/TarasevichV21 fatcat:vakobcncwrco5m32c4ywhlly4y