R. Ramachandran et al., PRECIPITATION DEVELOPMENT AND ELECTRIFICATION IN FLORIDA THUNDERSTORMCELLS DURING CONVECTION AND PRECIPITATION ELECTRIFICATION PROJECT/, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D1), 1996, pp. 1599-1619
Precipitation development and electrification in Florida thunderstorms
are observed using an instrumented aircraft and a multiparameter rada
r. A low concentration of raindrops initially develops in the updraft,
and these raindrops begin to freeze when they are carried above the 0
degrees C level. High concentrations of ice particles and downdrafts
soon appear in the -5 degrees to -10 degrees C regions of the cloud, w
here the aircraft penetrated, as do electric fields in the range of te
ns of kilovolts per meter. In a cell with relatively weak updrafts, dr
ops start to freeze at temperatures just below 0 degrees C. Although s
ignificant electric fields are measured by the aircraft, no lightning
is observed in this cell. In more vigorous cells, drops first begin to
freeze at temperatures between -5 degrees C and -10 degrees C. The el
ectric fields measured by the aircraft in these cells are similar in m
agnitude to those in the weaker cell. but lightning is observed in the
se more vigorous cells. The net charge in convective regions at altitu
des just above the aircraft penetration levels, 6-7 km, appears to be
negative.