The dynamics of NAO teleconnection pattern growth and decay

By S. Feldstein. 2003

275 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/a9181d1ea871382d09cc1fbf481c931e20e9e682

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Citations in the corpus

The Link between Rossby Wave Breakings and Weather Regime Transitions (2011, methodology): “These results are in good agreement with those of Feldstein (2003), who showed that the linear term is responsible for the NAO decay and more specifically its divergent part.”
Is the North Atlantic Oscillation a Breaking Wave (2004, background): “Also, because the model results of this study show that both NAO phases are preceded by high-frequency, synoptic-scale wave trains, the results of Feldstein (2003), together with those of this study, imply that the formation of the positive NAO phase is preceded by both high- and low-frequency wave…”
A Multifaceted Climatology of Atmospheric Blocking and Its Recent Linear Trend (2007, unknown): “A related issue is the possible linkage of the APV* trends to that of the North Atlantic Oscillation (NAO) since the latter can exhibit a life cycle of growth and decay within two weeks (Feldstein 2003) and this is comparable to that of major blocks.”
Breaking Waves at the Tropopause in the Wintertime Northern Hemisphere: Climatological Analyses of the Orientation and the Theoretical LC1/2 Classification (2007, background): “On the other hand it is suggested that the NAO pattern is significantly influenced by synoptic-scale breaking waves (Feldstein 2003; Benedict et al. 2004; Franzke et al. 2004).”
A New Rossby Wave–Breaking Interpretation of the North Atlantic Oscillation (2008, background): “This is consistent with Feldstein (2003), who showed that both high- and lowfrequency transient eddy fluxes contribute to the growth of NAO anomalies.”
Review of Tropical‐Extratropical Teleconnections on Intraseasonal Time Scales (2017, background): “Some of these climatic teleconnection patterns also exhibit variability on subseasonal time scales (Feldstein, 2003; Murakami, 1988; Wang, Wen, et al., 2016).”
Importance of Resolving Kuroshio Front and Eddy Influence in Simulating the North Pacific Storm Track (2017, background): “Previous studies have shown that accumulative effects of winter storms can contribute to large-scale mean atmospheric circulation changes (Benedict et al. 2004; Feldstein 2003; Riviere and Orlanski 2007; Vallis and Gerber 2008).”
The impact of the MJO on clusters of wintertime circulation anomalies over the North American region (2012, result): “Such results may be explained by the results of Feldstein (2003), who found that the positive NAO (which is highly correlated to the AO) is preceded by an upstream wave train located over North America and the northeast Pacific, whereas the negative NAO exhibits in-situ development.”
Dynamical feedbacks and the persistence of the NAO (2009, methodology): “Later, he demonstrated, using a reanalysis dataset, that the growth of the anomalous circulation associated with the NAO is driven by the eddy fluxes and that the divergence term is a major contributor to the NAO’s subsequent decay (Feldstein 2003).”