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The Tropical Cloud Population
R. A. Houze
Lecture, Indian Institute of Tropical Meteorology, Pune, 9 August 2010
Clouds in Low Latitudes
Lecture Sequence1. Basic tropical cloud types
2. Severe convection & mesoscale systems
3. Tropical cloud population
4. Convective feedbacks to large-scales
5. Monsoon convection
6. Diurnal variability
7. Clouds in tropical cyclones
Before Satellites
Small cumulus
Cumulus congestus
Cumulonimbus and mesoscale convective systems
Visual Observation
View from an aircraft flying over the South China Sea
“Hot tower hypothesis”
of
Riehl & Malkus 1958
Radiosonde Data
Satellite Observations
Large cloud shields
Large cloud shields
Circa 1970
Good:•Explained satellite pictures •Retained the hot tower notion •Included smaller clouds
Satellite view of the tropical cloud population
Not good:•Missing downdraft•No stratiform rain•Unrealistic scale separation
Radars
GATE 1974
GATE SHIP ARRAY
More Field Projects to Study Convection
BoB 1979
JASMINE1999
EPIC 2001
TEPPS1997
(Dashed: No sounding network)
Houze et al. (1980)
Post-GATE view of the tropical cloud population
STRATIFORMRAIN
MESOSCALE CONVECTIVE SYSTEMS (MCSs)
By the early 1980’sIdealized life cycle of tropical MCS
Houze 1982
Precipitation Radar in Space
The TRMM SatelliteThe TRMM Satellite
TRMM
Radar
Low altitude, low inclination orbit
TRMM Satellite InstrumentationTRMM Satellite Instrumentation
Kummerow et al, 1998
λ= 2 cmImportant! PR measures 3D structure of radar echoes
Knowledge of global rainfall before satellites measured rain from space
Combined satellite rainfall July 2000TRMM plus passive microwave sensors + other
Knowledge of global rainfall after TRMM & other satellites measured rain from space
How is tropical rain distributed by cloud size and type?
Schumacher & Houze 2003
2 Years of TRMM PR data
Large CbsMCSs
Smallisolated Cbs
How do the environments of these regimes differ?
Trade Wind Regime
Stratocumulus Regime
Trade Wind Regime
Indo/Pacific Warm Pool
Traditional conceptual view of mean meridional distribution of tropical convection
Simpson 1992
“Trimodal” distribution
Johnson et al. 1999
Conceptual
model based on TOGA COARE observations
Cu congestusSmall Cb
“Trimodal” distribution
Johnson et al. 1999
Evidence from TOGA COARE
soundingdata
“Trimodal” distribution
Hollars et al. 1999
Evidence
from Manus ARM cloud radar
observations
XMANUSMANUSMANUSMANUS
Tropical cloud population related to SST
SST Climatology (July)TRMM PR Deep Convective
TRMM PR Shallow, Isolated Convective
July SST
Land vs Ocean
TRMM view of Africa vis a vis the Atlantic
Rain Stratiform Rain Fraction
MCSs with large 85GHz ice scattering
Lightning
Cloud Radar in Space
Anvils of Mesoscale Convective Systems (MCSs)
Yuan and Houze 2010
1 2 3
Three steps of analysis of multi-sensor data
&(GEOPROF-2B)(TB11)
Yuan and Houze 2010
(GEOPROF-2B)(TB11)
MO
DIS
MO
DIS
CloudSat
Use MODIS and CloudSat to find threshold of thick high cloud
Yuan and Houze 2010
1-Find“cold centers”2-Use AMSR-E to find rain areas
Use 260 K threshold
Locate 1st closed contour
Use 1 mm/h threshold for rain rate
Yuan and Houze 2010
Associate pixels with nearest cold center
Define criterion for MCS that is reasonable for all these regions
Yuan and Houze 2010
TB11 = 220 Area > 2000 km2
account for most of the rainfall
Colors show rain amount
Size of cold cloud top
Tem
pera
ture
def
inin
g co
ld c
ente
r
Yuan and Houze 2010
“Connected” and “Separated” MCSs
Yuan and Houze 2010
MCSs Over the Whole Tropics
Yuan and Houze 2010
MCSs Over the Whole Tropics
Yuan and Houze 2010
Frequency of MCS anvils over tropics
Yuan and Houze 2010
Comparison of MCS anvils in different parts of the tropics
CloudSat data
Yuan and Houze 2010
Milestones in determining the tropical cloud population
Pre-satellite era
Hot towers and smaller clouds
Radars in field projects
MCSs, squall lines, stratiform precipitation
Precipitation radar in space
Patterns of convective, stratiform, shallow isolatedRelation to ocean & land
Cloud radar in space
Global distributions of MCSs & anvils
Clouds in Low Latitudes
Next
Lecture Sequence1. Basic tropical cloud types
2. Severe convection & mesoscale systems
3. Tropical cloud population
4. Convective feedbacks to large-scales
5. Monsoon convection
6. Diurnal variability
7. Clouds in tropical cyclones
This research was supported by NASA grants NNX07AD59G, NNX07AQ89G, NNX09AM73G, NNX10AH70G, NNX10AM28G,
NSF grants, ATM-0743180, ATM-0820586, DOE grant DE-SC0001164 / ER-6