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A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

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Characteristics of deep convection over <strong>the</strong> <strong>Amazon</strong>during LBA using GOES and PR/TRMM d<strong>at</strong>aT. InoueMeteorological Research Institutetinoue@mri-jma.go.jpABSTRACTLife cycle of deep convection and diurnal vari<strong>at</strong>ion of deep convectionover <strong>the</strong> <strong>Amazon</strong> are studied using <strong>the</strong> GOES-8 split window (11 and 12micron) d<strong>at</strong>a. Using <strong>the</strong> split window d<strong>at</strong>a we can classify optically thickcumulus type cloud and optically thin cirrus type cloud. The life cycleof deep convection is characterized as cumulus type cloud is dominantduring <strong>the</strong> developing stage and optically thin cirrus type cloud (anvil)is dominant during <strong>the</strong> decaying stage. Considering <strong>the</strong> cloud amount ofcumulus type cloud and cirrus type cloud <strong>with</strong>in <strong>the</strong> cloud area definedby <strong>the</strong> brightness temper<strong>at</strong>ure colder than 253K, we tried to define <strong>the</strong>stage of deep convection. Using <strong>the</strong> coincident and colloc<strong>at</strong>ed GOES andTRMM d<strong>at</strong>a, we compared <strong>the</strong> rain type observed by PR/TRMM and life stageof deep convection. There is a tendency th<strong>at</strong> convective rain is dominantduring <strong>the</strong> developing stage and str<strong>at</strong>iform rain is dominant during <strong>the</strong>decaying stage. The diurnal vari<strong>at</strong>ion of deep convection is also studiedusing <strong>the</strong> cloud type classified by <strong>the</strong> split window. The cloud amountpeak of cumulonimbus type cloud appears earlier than th<strong>at</strong> of cloud colderthan 253K. The local time of <strong>the</strong> peak of cumulonimbus cloud is closerto <strong>the</strong> peak of rainfall observ<strong>at</strong>ion by surface radar than <strong>the</strong> peak ofcloud colder than 253K.

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