A linkage between the North Atlantic Oscillation and its downstream development due to the existence of a blocking ridge

• Published in: Journal of Geophysical Research Vol. 116; no. D11
• Main Authors: Sung, Mi-Kyung, Lim, Gyu-Ho, Kug, Jong-Seong, An, Soon-Il
• Format: Journal Article
• Language: English
• Published: Washington, DC Blackwell Publishing Ltd 16.06.2011; American Geophysical Union
• Subjects: Atmosphere; blocking; Climate change; Earth; Earth sciences; Earth, ocean, space; Exact sciences and technology; Geophysics; NAO; phase asymmetry; Regions; Wave energy; Russian Federation; Eurasia; Atlantic Ocean; Europe; Siberia; North Atlantic; Northwest Atlantic; AN, North Atlantic; AN, North Atlantic, North Atlantic Oscillation; INW, Russia, Siberia; ANE, Europe; PNE, Eurasia; North Atlantic oscillation; Anticyclone; circulation; Wave train; growth; Vortex; low frequency; energy; Standing wave
• ISSN: 0148-0227; 2169-897X; 2156-2202; 2169-8996
• DOI: 10.1029/2010JD015006

In this work the spatial growth of the North Atlantic Oscillation (NAO) and its relationship to downstream development are examined. In contrast to positive NAO events, which are primarily initiated over the western North Atlantic, negative persistent NAO events tend to be preceded by a blocking ridge in the vicinity of northern Europe. This blocking ridge contributes to the growth of negative NAO events through a low‐frequency eddy interaction. It is also shown that a noticeable downstream development is dominant only for negative persistent NAO events that are preceded by the blocking ridge. While the blocking ridge exists over inland Eurasia, it induces anticyclonic circulation near the surface over Siberia. As the NAO grows, a stationary wave train that originates from the North Atlantic transfers wave energy downstream toward Siberia. The surface anticyclone is then reinforced by the wave train and begins to migrate eastward. This process explains the distinct impact of the negative NAO on the downstream Eurasian region. Key Points We find that negative NAO events tend to be preceded by a blocking ridge Noticeable downstream development is dominant only for ‐NAO with blocking ridge We document distinct role of blocking ridge in ‐NAO and downstream development