Mechanisms for the NAO Responses to the North Atlantic SST Tripole
By Shiling Peng, W. Robinson, Shuanglin Li. 2003
204 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a06004fb1a8748d617d4b78f002eaa94645424c3
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Paul J. Kushner
- Timothy J. Mosedale
- C. Deser
- M. Collins
- S. Hardiman
- Terence C. Mills
- David B. Stephenson
- Judah Cohen
In Global and Planetary Change
- Paul J. Kushner
- Timothy J. Mosedale
- C. Deser
- M. Collins
- S. Hardiman
- Terence C. Mills
- David B. Stephenson
- Judah Cohen
Citations in the corpus
- 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 (2004, background): “Recently, Peng et al. (2003) have proposed that nonlinear interactions between the anomalous heating and eddy-in- duced components of the flow can lead to asymmetries in the response to positive versus negative SST anomalies.”
- Granger Causality of Coupled Climate Processes: Ocean Feedback on the North Atlantic Oscillation (2006, background): “Many previous studies of ocean–atmosphere interaction in the North Atlantic region have highlighted the role of the SST tripole pattern (e.g., Bjerknes 1964; Deser and Timlin 1997; Czaja and Frankignoul 1999; Peng et al. 2003; Cassou et al. 2004).”
- The dynamical response to snow cover perturbations in a large ensemble of atmospheric GCM integrations. (2008, background): “Thus, we see over time the transition of the response from a thermally direct response in the onset phase to a dynamical annular mode response involving strong eddy forcing (Peng et al. 2003; Deser et al. 2007).”
- The Transient Atmospheric Circulation Response to North Atlantic SST and Sea Ice Anomalies (2007, unknown): “These transient eddy feedbacks may substantially modify the direct baroclinic response to anomalous diabatic heating (Hoskins and Karoly 1981; Hendon and Hartmann 1982) into an equivalent barotropic response that extends well beyond the region of forcing (Peng et al. 2003; Magnusdottir et al. 2004).”