The Midlatitude Continental Convective Clouds Experiment (MC3E)

Author:

Jensen M. P.1,Petersen W. A.2,Bansemer A.3,Bharadwaj N.4,Carey L. D.5,Cecil D. J.6,Collis S. M.7,Del Genio A. D.8,Dolan B.9,Gerlach J.2,Giangrande S. E.1,Heymsfield A.3,Heymsfield G.10,Kollias P.11,Lang T. J.6,Nesbitt S. W.12,Neumann A.13,Poellot M.13,Rutledge S. A.9,Schwaller M.10,Tokay A.14,Williams C. R.15,Wolff D. B.2,Xie S.16,Zipser E. J.17

Affiliation:

1. Brookhaven National Laboratory, Upton, New York

2. NASA Goddard Space Flight Center, Greenbelt, Maryland, and NASA Wallops Flight Facility, Wallops Island, Virginia

3. National Center for Atmospheric Research, Boulder, Colorado

4. Pacific Northwest National Laboratory, Richland, Washington

5. University of Alabama in Huntsville, Huntsville, Alabama

6. NASA Marshall Space Flight Center, Huntsville, Alabama

7. Argonne National Laboratory, Argonne, Illinois

8. NASA Goddard Institute for Space Studies, New York, New York

9. Colorado State University, Fort Collins, Colorado

10. NASA Goddard Space Flight Center, Greenbelt, Maryland

11. McGill University, Montreal, Quebec, Canada

12. University of Illinois at Urbana–Champaign, Urbana, Illinois

13. University of North Dakota, Grand Forks, North Dakota

14. University of Maryland, Baltimore County, Baltimore, and NASA Goddard Space Flight Center, Greenbelt, Maryland

15. University of Colorado, Boulder, Boulder, Colorado

16. Lawrence Livermore National Laboratory, Livermore, California

17. University of Utah, Salt Lake City, Utah

Abstract

Abstract The Midlatitude Continental Convective Clouds Experiment (MC3E), a field program jointly led by the U.S. Department of Energy’s Atmospheric Radiation Measurement (ARM) Program and the National Aeronautics and Space Administration’s (NASA) Global Precipitation Measurement (GPM) mission, was conducted in south-central Oklahoma during April–May 2011. MC3E science objectives were motivated by the need to improve our understanding of midlatitude continental convective cloud system life cycles, microphysics, and GPM precipitation retrieval algorithms. To achieve these objectives, a multiscale surface- and aircraft-based in situ and remote sensing observing strategy was employed. A variety of cloud and precipitation events were sampled during MC3E, of which results from three deep convective events are highlighted. Vertical structure, air motions, precipitation drop size distributions, and ice properties were retrieved from multiwavelength radar, profiler, and aircraft observations for a mesoscale convective system (MCS) on 11 May. Aircraft observations for another MCS observed on 20 May were used to test agreement between observed radar reflectivities and those calculated with forward-modeled reflectivity and microwave brightness temperatures using in situ particle size distributions and ice water content. Multiplatform observations of a supercell that occurred on 23 May allowed for an integrated analysis of kinematic and microphysical interactions. A core updraft of 25 m s−1 supported growth of hail and large raindrops. Data collected during the MC3E campaign are being used in a number of current and ongoing research projects and are available through the ARM and NASA data archives.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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