Comparison of the Life Cycles of the NAO Using Different Definitions

• Published in: Journal of climate 2007-12, Vol.20 (24), p.5992-6011
• Main Authors: Jia, XiaoJing, Derome, Jacques, Lin, Hai
• Format: Article
• Language: English
• Subjects: Atmosphere; Atmospherics; Climate; Climatology; Climatology. Bioclimatology. Climate change; Correlations; Definitions; Earth, ocean, space; Exact sciences and technology; External geophysics; Frequency distribution; General circulation models; Geopotential height; Life cycles; Meteorology; Meteors; Northern hemisphere; Polar environments; Polar regions; Principal components analysis; Time series; Vorticity
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/2007JCLI1408.1

This study investigates the North Atlantic Oscillation (NAO) on an intraseasonal time scale. The authors investigate the question of how the characteristics of NAO events are influenced by the choice of its definitions using daily NCEP–NCAR reanalysis data spanning 51 boreal winters. Four different NAO indexes are used in this study, including one station/gridpoint–based index and three pattern-based indexes. It is found that the NAO events obtained using pattern–based indexes are quite similar to each other, while some notable differences are observed when the NAO is defined using the station/gridpoint–based index (NAO1). The characteristics of the pattern-based NAO are found to be more antisymmetric for its two phases, including its time-averaged spatial structures, its lifetime distributions, and time-evolving spatial structures. The NAO1, on the other hand, reveals some asymmetric characteristics between the two phases. Emphasis is placed on comparing the characteristics of the NAO events obtained using the NAO1 index and one of the pattern-based indices, that is, NAO2. The time-averaged spatial structures for the NAO2 expand across more of the polar region than the NAO1. The positive NAO1 shows a wave train signal over the Pacific–North American region during the setup phase, while the negative NAO1 is found to develop more locally over northern Europe and the North Atlantic. The wave activity flux for the NAO2 is primarily in the zonal direction while for the NAO1, on the other hand, it is mostly concentrated over the North Atlantic with a pronounced southward component. The barotropic vorticity equation is used to examine the physical mechanisms that drive the life cycle of the NAO.