Dynamics of 2-Day Equatorial Waves
By P. Haertel, G. Kiladis. 2004
140 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/9695f87f717047f12d9c703299fdba53b09bf2cd
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Citations in the corpus
- Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “…embedded fast eastward propagating moist Kelvin waves and associated 2‐day westward propagating inertio‐gravity waves (S. S. Chen & Houze, 1997; Haertel & Kiladis, 2004; Hendon & Liebmann, 1994; Liebmann et al., 1997; Takayabu, 1994), westward propagating mixed Rossby‐gravity waves that are…”
- A New Multiscale Model for the MaddenJulian Oscillation (2005, background): “A recent study of two-day waves (Haertel and Kiladis 2004) shows, in that context, that the rigid lid approximation is an excellent one for capturing lower middle troposphere dynamics.”
- Madden‐Julian Oscillation (2005, background): “The 2-day disturbances are likely manifestations of the diurnal cycle of deep convection [Chen and Houze, 1997] and inertiogravity waves [Takayabu, 1994; Liebmann et al., 1997; Haertel and Kiladis, 2004].”
- Analysis of Convectively Coupled Kelvin Waves in the Indian Ocean MJO (2008, background): “In general, smaller-scale convective elements evolve similarly (e.g., Haertel and Kiladis 2004; Kiladis et al. 2005; and others).”
- Zonal and Vertical Structure of the Madden–Julian Oscillation (2005, methodology): “This evolution compares well with the progression of heating in two-day waves (Haertel and Kiladis 2004), which proceeds at a much faster pace (hours instead of days).”
- A Global High‐Resolution Mesoscale Convective System Database Using Satellite‐Derived Cloud Tops, Surface Precipitation, and Tracking (2021, background): “MCSs are often embedded within various tropical waves such as convectively coupled Kelvin waves (Haertel & Kiladis, 2004), synoptic easterly waves (Schumacher & Houze, 2006), and the Madden-Julian Oscillation (MJO; Moncrieff, 2010).”
- Convectively coupled equatorial waves (2009, methodology): “…data are not available for the COARE region, events were frequent enough during COARE that reasonable vertical structures can be obtained from the dense array of four times daily soundings taken during that experiment, using 1.5–3 day filtered Tb as a predictor [Haertel and Kiladis, 2004].”
- The mesoscale convection life cycle: building block or prototype for large-scale tropical waves? (2006, background): “…vastly greater than the size of individual cloud shields seen in satellite imagery, yet its flow fields approximately satisfy dispersion relations from linear equatorial wave theory, specifically the westward inertio-gravity wave—see also Haertel and Johnson (1998) and Haertel and Kiladis (2004).”
- A Moisture-Stratiform Instability for Convectively Coupled Waves (2008, methodology): “As discussed further in Appendix A and noted in many previous studies (e.g. Haertel and Kiladis, 2004), there is substantial compensation between adiabatic cooling and convective heating associated with the first mode, i.e. w1~J1.”
- Three-Dimensional Structure and Dynamics of African Easterly Waves. Part I: Observations (2006, result): “This structure also compares well to other equatorial waves observed by Wheeler et al. (2000), Straub and Kiladis (2002), and Haertel and Kiladis (2004).”