Structure and Properties of Madden–Julian Oscillations Deduced from DYNAMO Sounding Arrays

191 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Mechanisms of convective cloud organization by cold pools over tropical warm ocean during the AMIE/DYNAMO field campaign (2015, background): “This transition is generally associated with increasing convective activity and moistening of the mid-troposphere [Johnson and Ciesielski, 2013; Powell and Houze, 2013], characterized by the weakening of equatorward midlevel advection of dry air as the Rossby gyres from the preceeding MJO episode re”
The MJO as a Dispersive, Convectively Coupled Moisture Wave: Theory and Observations (2016, unknown): “Observational evidence by Benedict and Randall (2007), Johnson and Ciesielski (2013), and Adames and Wallace (2015) is qualitatively consistent the idea of Rossby waves producing damping within the moist region in the MJO.”
A Comparison of OLR and Circulation-Based Indices for Tracking the MJO (2014, background): “Eastward propagation of primarily negative OLR perturbations is dominant during DYNAMO, with two well-defined MJO events during October (MJO1) and November (MJO2; Y13; JC13).”
Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “The region to the east of MJO convection is characterized by enhanced lower‐tropospheric moisture anomalies (e.g., Johnson & Ciesielski, 2013; Kemball‐Cook & Weare, 2001; Kiladis et al., 2005; Sperber, 2003; Tian et al., 2010), warm sea surface temperature (SST; Hendon & Glick, 1997; Woolnough et…”