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The Tropical Cloud Population R. A. Houze Lecture, Indian Institute of Tropical Meteorology, Pune, 9 August 2010
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Clouds in Low Latitudes Lecture Sequence 1.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
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Before Satellites
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Small cumulus Cumulus congestus Cumulonimbus and mesoscale convective systems Visual Observation View from an aircraft flying over the South China Sea
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“Hot tower hypothesis” of Riehl & Malkus 1958 Radiosonde Data
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Satellite Observations
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Large cloud shields
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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
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Radars
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GATE 1974
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GATE SHIP ARRAY
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More Field Projects to Study Convection BoB 1979 JASMINE 1999 EPIC 2001 TEPPS 1997 (Dashed: No sounding network)
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Houze et al. (1980) Post-GATE view of the tropical cloud population STRATIFORM RAIN MESOSCALE CONVECTIVE SYSTEMS (MCSs)
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By the early 1980’s Idealized life cycle of tropical MCS Houze 1982
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Precipitation Radar in Space
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The TRMM Satellite TRM M Radar Low altitude, low inclination orbit
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TRMM Satellite Instrumentation Kummerow et al, 1998 = 2 cm Important! PR measures 3D structure of radar echoes
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Knowledge of global rainfall before satellites measured rain from space
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Combined satellite rainfall July 2000 TRMM plus passive microwave sensors + other Knowledge of global rainfall after TRMM & other satellites measured rain from space
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How is tropical rain distributed by cloud size and type?
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Schumacher & Houze 2003 2 Years of TRMM PR data Large Cbs MCSs Small isolated Cbs
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How do the environments of these regimes differ?
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Trade Wind Regime
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Stratocumulus Regime
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Trade Wind Regime
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Indo/Pacific Warm Pool
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Traditional conceptual view of mean meridional distribution of tropical convection Simpson 1992
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“Trimodal” distribution Johnson et al. 1999 Conceptual model based on TOGA COARE observations Cu congestus Small Cb
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“Trimodal” distribution Johnson et al. 1999 Evidence from TOGA COARE sounding data
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“Trimodal” distribution Hollars et al. 1999 Evidence from Manus ARM cloud radar observations X MANUSMANUS
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Tropical cloud population related to SST
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SST Climatology (July) TRMM PR Deep Convective TRMM PR Shallow, Isolated Convective July SST
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Land vs Ocean
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TRMM view of Africa vis a vis the Atlantic Rain Stratiform Rain Fraction MCSs with large 85 GHz ice scattering Lightning
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Cloud Radar in Space
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Anvils of Mesoscale Convective Systems (MCSs) Yuan and Houze 2010
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123 Three steps of analysis of multi-sensor data & (GEOPROF-2B) (TB11) Yuan and Houze 2010 (GEOPROF-2B) (TB11)
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MODIS CloudSat Use MODIS and CloudSat to find threshold of thick high cloud Yuan and Houze 2010
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1-Find“cold centers” 2-Use AMSR-E to find rain areas Use 260 K threshold Locate 1 st closed contour Use 1 mm/h threshold for rain rate Yuan and Houze 2010 Associate pixels with nearest cold center
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Define criterion for MCS that is reasonable for all these regions Yuan and Houze 2010
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TB11 = 220 Area > 2000 km 2 account for most of the rainfall Colors show rain amount Size of cold cloud top Temperature defining cold center Yuan and Houze 2010
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“Connected” and “Separated” MCSs Yuan and Houze 2010
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MCSs Over the Whole Tropics Yuan and Houze 2010
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MCSs Over the Whole Tropics Yuan and Houze 2010
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Frequency of MCS anvils over tropics Yuan and Houze 2010
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Comparison of MCS anvils in different parts of the tropics CloudSat data Yuan and Houze 2010
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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 isolated Relation to ocean & land Cloud radar in space Global distributions of MCSs & anvils
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Clouds in Low Latitudes Next Lecture Sequence 1.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
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This research was supported by NASA grants NNX07AD59G, NNX07AQ89G, NNX09AM73G, NNX10AH70G, NNX10AM28G, NSF grants, ATM-0743180, ATM-0820586, DOE grant DE-SC0001164 / ER-6
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