The Effects of North Atlantic SST and Sea Ice Anomalies on the Winter Circulation in CCM3. Part II: Direct and Indirect Components of the Response
By C. Deser, Guðrún Magnúsdóttir, Ramalingam Saravanan, A. Phillips. 2004
330 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/fd2f7767124dbf110a04c7375f95da61f9c2cc29
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In Atmospheric Science
- T. Woollings
- B. Hoskins
- M. Blackburn
- P. Berrisford
- Hisashi Nakamura
- Zhengyu Liu
- M. Alexander
- Grant Branstator
In Global and Planetary Change
- T. Woollings
- B. Hoskins
- M. Blackburn
- P. Berrisford
- Hisashi Nakamura
- Zhengyu Liu
- M. Alexander
- Grant Branstator
In Oceanography
- T. Woollings
- B. Hoskins
- M. Blackburn
- Hisashi Nakamura
- M. Alexander
- Zhengyu Liu
- P. Berrisford
- A. Gritsun
Citations in the corpus
- Structure and dynamics of decadal anomalies in the wintertime midlatitude North Pacific ocean–atmosphere system (2016, background): “…such as the Pacific Decadal Oscillation (PDO) over North Pacific and the North Atlantic Oscillation (NAO) over North Atlantic (Trenberth 1990; Graham et al. 1994; Kushnir 1994; Minobe 1997; Mantua et al. 1997; Enfield and Mestas-Nunez 1999; Zhu and Yang 2003a; Deser et al. 2004; Fang et al. 2006).”
- Climate Response Using a Three-Dimensional Operator Based on the Fluctuation–Dissipation Theorem (2007, methodology): “The tool we will consider is made possible by the fluctuation–dissipation theorem (FDT), which was obtained in different variations by Nyquist (1928), Callen and Welton (1951), Kraichnan (1959), Kubo (1957), and Deker and Haake (1975).”
- A New Rossby Wave–Breaking Interpretation of the North Atlantic Oscillation (2008, background): “Such responses occur in the experiments of Deser et al. (2004) and in the shift of the NAO pattern seen by Ulbrich and Cristoph (1999).”
- Atmospheric bridge, oceanic tunnel, and global climatic teleconnections (2007, background): “The resulting eddy momentum fluxes drive a large-scale equivalent barotropic response [Peng and Whitaker, 1999], which often resembles the internal modes of atmospheric variability [Peng and Robinson, 2001; Alexander et al., 2004a; Deser et al., 2004a].”
- Importance of Resolving Kuroshio Front and Eddy Influence in Simulating the North Pacific Storm Track (2017, background): “…oceanic eddies on the atmosphere, which partly arises from the nonlinearity in the Clausius–Clapeyron saturation vapor pressure relationship that gives a disproportionately larger impact on boundary layer humidity from warm ocean eddies than cold eddies (Deser et al. 2004; Ma et al. 2015).”
- The Transient Atmospheric Circulation Response to North Atlantic SST and Sea Ice Anomalies (2007, neutral): “…on the location of the SST forcing, the response may project onto the dominant modes of internal atmospheric variability thereby changing their frequency of occurrence (Peng and Robinson 2001; Hall et al. 2001; Peng et al. 2003; Magnusdottir et al. 2004; Deser et al. 2004; Cassou et al. 2007).”