_id,doi,title
15047,10.1126/sciadv.adj6801,Intensification of daily tropical precipitation extremes from more organized convection
14453,10.1029/2022MS003477,Extreme precipitation in tropical squall lines
14654,10.1029/2023MS003726,Assessing memory in convection schemes using idealized tests
14752,10.1029/2023av000880,"How moisture shapes low‐level radiative cooling in subsidence regimes"
14773,10.1063/pt.3.5234,The cloud dynamics of convective storm systems
14853,10.1002/9781119700357.ch8,"Mechanisms for the Self‐Organization of Tropical Deep Convection"
14863,10.5194/egusphere-egu23-6157,Intensification mechanisms of tropical cyclones
14864,10.5194/egusphere-egu23-6166,Measuring spontaneous charging of single aerosol particles
14865,10.5194/egusphere-egu23-4968,Evaluating memory properties in convection schemes using idealised tests
14866,10.5194/egusphere-egu23-15870,Extreme precipitation in tropical squall lines
14991,10.5281/ZENODO.7757041,Data-assessing memory in convection schemes using idealized tests
10656,10.1146/annurev-fluid-022421-011319,Spontaneous aggregation of convective storms
10653,10.1029/2021GL095184,Shear-convection interactions and orientation of tropical squall lines
12107,10.1029/2022GL100624,"Precipitating fraction, not intensity, explains extreme coarse-grained precipitation Clausius-Clapeyron scaling with sea surface temperature over tropical oceans"
9151,10.1029/2020ms002256,"Distortions of the rain distribution with warming, with and without self‐aggregation"
9124,10.5194/essd-2020-269,Atmospheric radiative profiles during EUREC4A
9125,10.1029/2020ms002164,"Self‐aggregation of convective clouds with interactive sea surface temperature"
9126,10.1029/2020ms002106,"What controls the water vapor isotopic composition near the surface of tropical oceans? Results from an analytical model constrained by large‐eddy simulations"
9127,10.1007/s10113-020-01659-w,How warmer and drier will the Mediterranean region be at the end of the twenty-first century?
9128,10.1088/1748-9326/ab7130,"Response of precipitation extremes to warming: What have we learned from theory and idealized cloud-resolving simulations, and what remains to be learned?"