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