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Title: Polarimetric signatures in the stratiform region of a mesoscale convective system

Journal Article · · Journal of Applied Meteorology; (United States)
; ;  [1];  [2];  [3];  [4]
  1. National Severe Storms Lab., Norman, OK (United States)
  2. Indian Institute of Science, Bangalore (India)
  3. Colorado State Univ., Fort Collins (United States)
  4. Pennsylvania State Univ., University Park (United States)

Four polarimetric measurements were collected in the stratiform region of a mesoscale convective system. The four are the reflectivity factor, the differential reflectivity, the correlation coefficient between orthogonal copolar echoes, and the differential propagation constant. Most striking is a signature of large aggregates (about 10 mm in size) seen in the differential phase through the melting layer. Another significant feature is an abrupt notch in the correlation coefficient that occurs towards the bottom of the bright band. Aircraft observations and a one-dimensional cloud model are used to explain some polarimetric measurements and to infer the presence of aggregates, graupel, and supercooled cloud water -in the stratiform region. These unique observations and model data provide inferences concerning the presence of graupel and the growth of large aggregates in the melting layer. 25 refs., 9 figs., 1 tab.

OSTI ID:
6531120
Journal Information:
Journal of Applied Meteorology; (United States), Vol. 32:4; ISSN 0894-8763
Country of Publication:
United States
Language:
English