Insights Into Precipitation Processes As Revealed By Profiling Radar, Disdrometer and Aircraft Observations During The MC3E Campaign.
Scott E Giangrande, Brookhaven National Laboratory, Environmental Science and Technologies Department, Upton, United States, Tami Fairless, Brookhaven National Laboratory, Upton, NY, United States, Aaron Bansemer, NCAR, Boulder, CO, United States, Matthew R Kumjian, The Pennsylvania State University, Department of Meteorology and Atmospheric Science, University Park, PA, United States and Alexander Ryzhkov, NOAA/OAR/National Severe Storms Laboratory, Norman, OK, United States
Contact First Author: Scott E Giangrande; scott.giangrande@gmail.com
Previously Published Material: 2014 AGU Fall Meeting Poster; However, was unable to attend;
English Abstract:
The Midlatitude Continental Convective Clouds Experiment (MC3E) was a collaborative campaign led by the National Aeronautic and Space Administration’s (NASA’s) Global Precipitation Measurement (GPM) mission and the U.S. Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) program. This campaign was held at the DOE ARM Southern Great Plains (SGP) Central Facility (CF) in north-central Oklahoma, with the programs joining forces to deploy an extensive array of airborne, radiosonde and ground-based instrumentation towards an unprecedented set of deep convective environment and cloud property observations. An overarching motivation was to capitalize on the wealth of aircraft observations and new multi-frequency dual-polarization radars to provide insights for improving the treatments of cloud processes in convective models.
This study considers a coupled aircraft, radar and surface disdrometer approach for identifying key cloud processes and linking those to possible radar-based microphysical fingerprints and/or cloud properties. Our emphasis is on the MC3E observations from April 27th, 2011 and collected during successive aircraft spirals over the column of the ARM CF. We investigate the usefulness of radar to inform on processes including aggregation and riming as viewed by vertically-pointing ARM wind profiler (915 MHz) and cloud radar Doppler spectral observations (35 GHz). Corresponding dual-polarization radar signatures from the nearby cm-wavelength radar are also consulted for complementary insights. For this event, the successive Citation II aircraft spirals through the melting layer and associated ground observations indicate a fortunate capture of the transition from a region of weak embedded updrafts and riming to one favoring aggregation processes more typical of the trailing stratiform shield of this event.
