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CloudSat-CALIPSO-AMSR-E data document sensitivity of tropical
convection to humidity during the Madden-Julian Oscillation
Large-scale
averages
Single
footprints
Observations
AMSR-E
GISS GCM
Weaker entrainment
Stronger entrainment
Context: GCMs poorly
simulate the MJO because
their convection schemes are
insensitive to tropospheric
humidity.
CloudSat/CALIPSO/AMSR-E
provides the first global direct
detection of convection depth,
while AMSR-E gives
simultaneous water vapor.
GEOPROF-LIDAR data were
accumulated over the
developing phase of 10 MJOs.
Left panels: A-train data show transition from shallow to deep convection at intermediate
column water vapor amounts (50-68 mm), but with all depths possible at these values
depending on details of the humidity profile.
Right panels: GISS GCM shallow-deep convection transition occurs too soon when too
little dry air is entrained into clouds, but gets the correct transition with strong entrainment.
Del Genio et al. (2012), Journal of Climate
Cloudsat/calipso