The Dynamical Relationship between Subtropical and Eddy-Driven Jets.
By Sukyoung Lee, Hyun-kyung Kim. 2003
289 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a6c0bc09d1395880031beea2b11f539ff5fbaae7
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Citations in the corpus
- Breaking Waves at the Tropopause in the Wintertime Northern Hemisphere: Climatological Analyses of the Orientation and the Theoretical LC1/2 Classification (2007, background): “For example, cyclonic life cycles are observed for both double jet (Shapiro et al. 1998) and single jet ( Lee and Kim 2003 ) settings.”
- Impact of stratospheric ozone on Southern Hemisphere circulation change: A multimodel assessment (2010, background): “It is also known that the extratropical jet, especially the summer hemisphere jet, is largely driven by baroclinic eddies [ Lee and Kim , 2003] and located at the latitude of maximum eddy momentum flux convergence in the upper troposphere [e.g., Son and Lee , 2005, Figure 1].”
- The relationship between the ITCZ and the Southern Hemispheric eddy‐driven jet (2013, background): “Subtropical jet strengthening is thus consistent with larger vertical wind shears, and therefore increasing baroclinicity and Eady growth rates near the subtropics [see e.g., Lee and Kim, 2003; Brayshaw et al., 2008].”
- Variability of the North Atlantic eddy‐driven jet stream (2010, unknown): “…with the behaviour in the South Pacific in the vicinity of the split jet stream (Figure 16f), and also with model results which suggest two distinct states depending on whether or not the subtropical and eddy-driven jets are separated ( Akahori and Yoden 1997; Lee and Kim 2003; Chan and Plumb 2009).”
- On the importance of midlatitude oceanic frontal zones for the mean state and dominant variability in the tropospheric circulation (2008, background): “Their transport of westerly momentum from the subtropics maintains a deep westerly jet-stream in midlatitudes [Lee and Kim, 2003], called the polar-front jet (PFJ).”
- Observed Associations Among Storm Tracks, Jet Streams and Midlatitude Oceanic Fronts (2013, background): “Thus, a westerly jet with modest core velocity bears an eddy-driven nature, a characteristic of a polar-front jet [Lee and Kim, 2003].”
- The Storm-Track Response to Idealized SST Perturbations in an Aquaplanet GCM (2008, methodology): “This difference is consistent with the weakening of the tropically driven component of the subtropical jet in experiment 3K30 , which provides a less fertile region for storm growth immediately on the poleward side of the subtropical jet (Lee and Kim 2003).”
- Rossby Wave Packets on the Midlatitude Waveguide—A Review (2018, background): “On Earth, there are essentially two jet streams: the subtropical jet and the extratropical, eddy-driven jet [Lee and Kim (2003) discuss the relevant dynamics].”
- Mechanisms of Hemispherically Symmetric Climate Variability (2003, background): “7 This is consistent with our expectation that eddy-driven anomalies will extend to the surface, while the anomalies driven by tropical heating will be largest in the upper troposphere (Lee and Kim 2003).”
- A consistent poleward shift of the storm tracks in simulations of 21st century climate (2005, methodology): “Due to the feedback between the storm tracks and the zonal mean flow, the cause of the poleward shift cannot be sorted out by diagnostic analysis alone; this will require additional model experiments, perhaps using an idealized model [e.g., Lee and Kim, 2003 ].”