Interactive comment on “Aerosols’ influence on the interplay between condensation, evaporation and rain in warm cumulus cloud” by O. Altaratz

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Aerosols’ influence on the interplay between condensation, evaporation and rain in warm cumulus cloud

1 Department of Environ. Sciences Weizmann Institute, Rehovot, Israel 2 Soreq Nuclear Research Center, Yavne, Israel 3 Department of Physics, Michigan Technological University, Houghton, Michigan, USA 4 NOAA Earth System Research Laboratory, Boulder, Colorado, USA 5 Department of Geophysics and Planetary Sciences, Tel Aviv University, Tel Aviv, Israel 6 Department Appl Meteorol. Nanjing Univ In...

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Convective cloud formation and evolution strongly depend on environmental temperature and humidity profiles. The forming clouds change the profiles that created them by redistributing heat and moisture. Here we show that the evolution of the field's thermodynamic properties depends heavily on the concentration of aerosol, liquid or solid particles suspended in the atmosphere. Under polluted con...

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Growth of Cloud Droplets in a Turbulent Environment

Motivated by the need to resolve the condensation-coalescence bottleneck in warm rain formation, a significant number of studies have emerged in the past 15 years concerning the growth of cloud droplets by water-vapor diffusion and by collision-coalescence in a turbulent environment.With regard to condensation, recent studies suggest that small-scale turbulence alone does not produce a signific...

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Aerosol Effects on Cumulus Congestus Population over the Tropical Pacific: A Cloud-Resolving Modeling Study

This study examines the significance of aerosol serving as cloud condensation nuclei (CCN) in modulating strengths of tropical maritime convection. Through a Tropical Ocean Global Atmosphere Couple Ocean̶Atmosphere Response Experiment (TOGA COARE) case study using a cloud-resolving model (the Goddard Cumulus Ensemble Model with a horizontal mesh interval of 750 m) and a detailed spectral bin mic...

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Interactive comment on “Aerosol concentrations determine the height of warm rain and ice initiation in convective clouds over the Amazon basin” by Ramon Campos Braga et al

Reviewer’s text: A strength of this paper is the presentation of cloud in-situ observations that addresses the question of how convective clouds are influenced by changing the concentration of aerosols. The authors have determined that the height of rain initiation given by D_i is approximately 5 * the number concentration of cloud droplets at cloud base, N_d. This type of study is needed for d...

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تاریخ انتشار 2007