Mechanisms of Hemispherically Symmetric Climate Variability
By R. Seager, N. Harnik, Y. Kushnir, W. Robinson, Jennifer Miller. 2003
436 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/ebef7a4554fbea0c2d374b0ea0311a1bb48b2ecf
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Citations in the corpus
- The Response of Tropospheric Circulation to Perturbations in Lower-Stratospheric Temperature (2005, positive): “In a study of the extratropical response to tropical forcing that is associated with ENSO, Seager et al. (2003) observed a similar relationship to that found here between anomalous eddy forcing and perturbations of the zonal mean state.”
- Width of the Hadley cell in simple and comprehensive general circulation models (2007, background): “…physical effects, such as changes in phase speed spectra (Chen and Held, submitted manuscript, 2007), tropopause height [Lorenz and DeWeaver, 2007], and subtropical wind changes [Seager et al., 2003; Seager et al., 2005] should not be ruled out as factors that can influence the Hadley cell width.”
- Phase Speed Spectra and the Latitude of Surface Westerlies: Interannual Variability and Global Warming Trend (2008, background): “…changes can be roughly explained by the impact of subtropical zonal wind anomalies on the equatorward propagation and absorption of midlatitude eddies near their critical latitudes, and subsequently on the eddy-driven extratropical circulation (Chang 1995, 1998; Robinson 2002; Seager et al. 2003).”
- The relationship between the ITCZ and the Southern Hemispheric eddy‐driven jet (2013, methodology): “This happens because the Hadley circulation controls the strength of the subtropical jet through the meridional advection of momentum in the upper tropical troposphere [Chang, 1995, Seager et al., 2003].”
- Impact of ENSO on the Atmospheric Variability over the North Atlantic in Late Winter—Role of Transient Eddies (2012, neutral): “tions (e.g., Chang 1998; Seager et al. 2003; Lau et al. 2005; Seager et al. 2010).”
- Energetic Constraints on the Position of the Intertropical Convergence Zone (2013, background): “At the same time, the Hadley circulation is narrower and stronger, resembling qualitatively (albeit not quantitatively) El Ni ~ no conditions on Earth (Seager et al. 2003).”