Large-Scale Meteorology and Deep Convection during TRMM KWAJEX*

By A. Sobel, Sandra E. Yuter, Chris Bretherton, G. Kiladis. 2004

152 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/cf0305b17620891b7fb7325333e56936baa361a0

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

1. E. Maloney
2. A. Sobel
3. Andrew J. Majda
4. P. Roundy
5. K. Straub
6. D. Frierson
7. G. Kiladis
8. M. Wheeler

In Global and Planetary Change

1. E. Maloney
2. A. Sobel
3. Andrew J. Majda
4. P. Roundy
5. K. Straub
6. D. Frierson
7. G. Kiladis
8. M. Wheeler

Citations in the corpus

• A Cumulus Parameterization with State-Dependent Entrainment Rate. Part I: Description and Sensitivity to Temperature and Humidity Profiles (2010, background): “…with many observational studies (Numaguti et al. 1995; Brown and Zhang 1997; Sherwood 1999; Sherwood and Wahrlich 1999; Bretherton et al. 2004b; Sobel et al. 2004; Biasutti et al. 2006; Peters and Neelin 2006; Takayabu et al. 2006; Neelin et al. 2008) and CRM results (Tompkins 2001;…”
• Large Scale Dynamics of Precipitation Fronts in the Tropical Atmosphere: A Novel Relaxation Limit (2004, background): “observational data which correlates the precipitation in the tropics with the humidity content [39].”
• Modelling tropical atmospheric convection in the context of the weak temperature gradient approximation (2005, methodology): “1301 This method is in widespread use (see, e.g., Sui et al. 1994; Grabowski et al. 1996, 1999; Grabowski et al. 1998; Xu and Randall 1999).”
• Convectively coupled equatorial waves (2009, background): “In addition, on synoptic time scales characteristic of CCEWs, CAPE tends to peak prior to convective initiation and is more often negatively correlated with the deepest convection [Sherwood, 1999; Straub and Kiladis, 2003c; Sobel et al., 2004], counter to the assumptions of SQE.”
• An Idealized Semi-Empirical Framework for Modeling the Madden–Julian Oscillation (2012, background): “…controlling convection while the upper-tropospheric water vapor is expected to vary more as a passive response to convection (e.g., Sherwood 1999; Sobel et al. 2004), so one could argue that for the model to capture that feedback it should weight lower-level advection more heavily. c. Model…”