- A13A-03: Cloud Edge Entrainment Increases the Local Proportion of Large Droplets Through Slower Phase-Relaxation: Results from Airborne Holography and High Resolution LES
-
NOLA CC
Author(s):Generic 'disconnected' Message
Elise Rosky, NSF National Center for Atmospheric Research (First Author, Presenting Author)
Raymond Shaw, Michigan Technological University
Hugh Morrison, NSF NCAR, MMM Laboratory
Kamal Kant Chandrakar, National Center for Atmospheric Research
Will Cantrell, Michigan Technological University
Sarah Woods, National Center for Atmospheric Research
Aaron Bansemer, NCAR
Advanced modeling and observational techniques are used to observe the evolution of cloud droplet sizes in cumulus clouds. Observations are collected by flying a research aircraft into cumulus clouds, with instrumentation attached to the wings to measure cloud droplet sizes. A holographic instrument (HOLODEC) is used, which samples thousands of droplets in one instant to provide fine-scale spatial resolution. High resolution Large Eddy Simulation (LES) with advanced representation of cloud droplets is used to simulate a cumulus congestus cloud in great detail.We find that although there are fewer droplets and smaller liquid water content in regions where dry air has been mixed into the cloud, the droplets that are present trend towards larger diameters than those in the undiluted part of the cloud. We use theoretical equations for cloud droplet growth rates to explain this observation. These findings contribute to a more complete understanding of how clouds develop, and may be relevant to the development of drizzle and precipitation.
Scientific DisciplineNeighborhoodType
Enter Note
Go to previous page in this tab
Session


