Further Analysis and Parameterization of Cloud MicrophysicalProcesses
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"Warm rain" in cloud physics refers to the development of                  precipitation in clouds in the absence of ice crystals.  Cloud                  droplets grown primarily through coalescence.  The droplet size                 spectra observed in nature have shown both bi-modal and tri-modal                                                                                               distributions.  Professor Brown has successfully explained the                  cause of such distributions by modeling both coalescence and the                                                                                                breakup process when droplets collide.  Under this grant                        Professor Brown will further consider the effects of evaporation                                                                                                and the initial droplet size spectra in the evolution of the                    spectra.  Since convective cloud models frequently cannot                       explicitly take into consideration the complex coalescence and                  collision-induced breakup, a refined parameterization, hence                    professor Brown's work, becomes even more important.
{'FirstName': 'Philip', 'LastName': 'Brown', 'PI_MID_INIT': 'S', 'PI_SUFX_NAME': 'Jr.', 'PI_FULL_NAME': 'Philip S Brown', 'EmailAddress': 'PBROWN@TRINCC', 'NSF_ID': '000118260', 'StartDate': '05/01/1988', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
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[{'Code': '1522', 'Text': 'PHYSICAL METEOROLOGY'}, {'Code': '9120', 'Text': 'CROSS-DIRECTORATE PROGRAMS'}]
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