CORRIGENDUM of the MJO Transition from Shallow to Deep Convection in Cloudsat-Calipso Data and GISS GCM Simulations

By A. D. Del Genio, Yonghua Chen, Daehyun Kim, M. Yao. 2012

185 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/e1b8ed4a8c678abad57dfba077b2fd9e1c980964

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. C. DeMott
3. N. Klingaman
4. Chidong Zhang
5. Hai Lin
6. Daehyun Kim
7. Á. Adames
8. Xianan Jiang

In Global and Planetary Change

1. E. Maloney
2. C. DeMott
3. N. Klingaman
4. Chidong Zhang
5. Hai Lin
6. Daehyun Kim
7. Á. Adames
8. Xianan Jiang

Citations in the corpus

• Mechanisms of convective cloud organization by cold pools over tropical warm ocean during the AMIE/DYNAMO field campaign (2015, background): “To the first-order, convective cloud-top heights vary with large-scale PW in a nonlinear fashion [see Del Genio et al., 2012; their Figure 4].”
• Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, methodology): “The latent and radiative heating products based on the TRMM (Jiang et al., 2009, 2011; Ling & Zhang, 2011; Masunaga et al., 2006; W.‐K. Tao et al., 2006), moisture and temperature estimates based on the Atmospheric Infrared Sounder (AIRS; Tian, Waliser, Fetzer, Lambrigtsen, et al., 2006; Tian et al.”
• Scale Interactions between the MJO and the Western Maritime Continent (2016, unknown): “…of fast physical processes, such as convection (Holloway et al. 2012), the transition from shallow to deep convection that coincides with the gradual moistening of the troposphere prior to the active MJO phase (Del Genio et al. 2012), and the interaction with the upper ocean (Tseng et al. 2015).”
• Tracking Pulses of the Madden–Julian Oscillation (2013, methodology): “For example, the aerosol measurement at Revelle indicates that the passage of MJO convection had a major impact on aerosol number, size and composition, and there was an aerosol regime change before and after convectively active episodes (DeWitt et al. 2013).”
• Structure and Properties of Madden–Julian Oscillations Deduced from DYNAMO Sounding Arrays (2013, methodology): “Low-level convergence, divergence aloft, and upward vertical motion progressively deepened with time in October, suggesting an evolution from shallow cumulus and congestus to deep convection with this event, as indicated by past studies (Johnson et al. 1999; Kikuchi and Takayabu 2004; Mapes et al. 2”