scholarly journals SENSING THE CORRELATION BETWEEN ATMOSPHERIC TELECONNECTION PATTERNS AND SEA ICE EXTENT: MICROS TECHNOLOGY “GEOMATH”

2014 ◽  
Vol 3 (2) ◽  
pp. 16-19
Author(s):  
A. V. Glushkov ◽  
V. N. Khokhlov ◽  
Y. Y. Bunyakova ◽  
A. A. Svinarenko ◽  
T. V. Solonko
Keyword(s):  
Sea Ice ◽  
Sea Ice Extent ◽  
Atmospheric Teleconnection ◽  
Teleconnection Patterns ◽  
Atmospheric Teleconnection Patterns

scholarly journals The Wintertime Wind Stress Curl Field in the North Atlantic and Its Relation to Atmospheric Teleconnection Patterns

2010 ◽  
Vol 67 (5) ◽  
pp. 1687-1694 ◽  
Author(s):  
Shusaku Sugimoto ◽  
Kimio Hanawa
Keyword(s):  
Wind Stress ◽  
North Atlantic ◽  
Wind Stress Curl ◽  
Atlantic Sector ◽  
Atmospheric Teleconnection ◽  
Maximum Covariance Analysis ◽  
Teleconnection Patterns ◽  
The North ◽  
The North Atlantic ◽  
Atmospheric Teleconnection Patterns

Abstract Adopting a rotated empirical orthogonal function (REOF) analysis and a maximum covariance analysis (MCA), characteristics of the wintertime wind stress curl (WSC) anomaly field in the North Atlantic are investigated. In terms of both temporal variation and spatial distribution, the first four leading modes of WSC show a one-to-one relation with four atmospheric teleconnection patterns over the North Atlantic sector: the North Atlantic Oscillation (NAO) and the east Atlantic (EA), tropical–Northern Hemisphere (TNH), and Pacific–North American (PNA) patterns. These four patterns characterize the WSC variations over the different regions in the North Atlantic: NAO and EA over the eastern side of the basin, TNH over the central part of the basin, and PNA over the western side of the basin.

Sign in / Sign up

Export Citation Format

Share Document