Mixed Rossby–Gravity Waves and Western Pacific Tropical Cyclogenesis. Part I: Synoptic Evolution
By Michael J. Dickinson, J. Molinari. 2000
218 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/c1e371182c231f58849189f6c077867bb5ecbe7c
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Citations in the corpus
- Analysis of Convectively Coupled Kelvin Waves in the Indian Ocean MJO (2008, background): “…Rossby waves (Kiladis and Wheeler 1995; Wheeler et al. 2000; Roundy and Frank 2004b), mixed Rossby–gravity waves (e.g., Hendon and Lieb-mann 1991; Dickinson and Molinari 2002), easterly waves or tropical-depression-type disturbances, west-ward inertio-gravity waves, and tropical cyclones…”
- The Madden-Julian Oscillation, Barotropic Dynamics, and North Pacific Tropical Cyclone Formation. Part I: Observations. (2001, background): “Equatorial western Pacific mixed-Rossby gravity waves are characterized by decreased phase speed and wavelength, and increased amplitude during periods of wave accumulation associated with MJO low-level convergence (Dickinson 2000).”
- Cluster Analysis of Typhoon Tracks. Part II: Large-Scale Circulation and ENSO (2007, background): “Differences in landfall patterns in different regions of Asia during ENSO cycles have been discussed in several studies (e.g., Saunders et al. 2000; Elsner and Liu 2003; Wu et al. 2004).”
- Tropical cyclogenesis in a tropical wave critical layer: easterly waves (2008, background): “…(mixed) Rossby-gravity waves of the central and far eastern Pacific Oceans (Hendon and Liebmann, 1991; Dunkerton, 1993; Dunkerton and Baldwin, 1995; Dickinson and Molinari, 2002; Molinari 2004); and 3. the so-called “tropical depression” disturbances of the western tropical Pacific (Liebmann and…”
- Modulation of South Indian Ocean Tropical Cyclones by the Madden–Julian Oscillation and Convectively Coupled Equatorial Waves (2006, background): “Except for the work of Dickinson and Molinari (2002), however, who found an association between TCs and MRG waves in the western Pacific, little can be found pub- lished in the literature on TC modulation by the equatorial waves.”
- Large-Scale Meteorology and Deep Convection during TRMM KWAJEX* (2004, methodology): “This is expected for MRG waves in this region based on previous work using more sophisticated analysis techniques (Liebmann and Hendon 1990; Dunkerton and Baldwin 1995; Dickinson and Molinari 2002 ), but is visible here with no temporal filtering or other processing of any kind.”
- Tropical Intraseasonal Variability in 14 IPCC AR4 Climate Models. Part I: Convective Signals (2006, background): “…equatorial waves mentioned above also strongly affect the tropical weather, for example, the occurrence of westerly wind burst events (e.g., Kiladis et al. 1994; Hartten 1996) and the formation of tropical cyclones (e.g., Dickinson and Molinari 2002; Goswami et al. 2003; Bessafi and Wheeler 2006).”
- A Climatology of Waves in the Equatorial Region (2004, background): “These wave modes may also contribute to the weather by affecting tropical cyclogenesis (e.g., Dickinson and Molinari 2002), and we are currently pursuing research in this area.”