Menu
Top page
Compliments radar
Min temperature
Anvil growth
Storm top dynamics
Equilibrium temp
Phase change
RFD's
Anvil-induced boundaries
Storm morphology
Future hypotheses
|
Satellite evidence of Rear Flank Downdrafts (RFD)?
Small areas of 6.7µm darkening have often been observed just upstream of
mature strong/severe storms in highly sheared environments. To date, there
are no formal studies linking these darkbands to the development of Rear
Flank Downdrafts.
However, consider the image displayed below. The flow through these
watervapor darkbands most likely conserves its potential temperature and
moisture. Therefore the darkening must be a result of subsidence in a
layer. Whether this darkening can produce enough of a vertical displacement
to initiate or assist the development of a RFD is not known. However, the
mechanisms that lead to the development of an RFD is still open to question.
|