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Satellite Radar Studies of Extreme Convective
Storms
?Himalayas
Andes
Rockies
New Fellows Presentation, AGU, San Francisco, 5 December 2012
Robert A. Houze, Jr.University of Washington
Radars in Space
TRMM1997-
CloudSat
2006-
Typical Tropical Convective Cloud Population
TRMM
2 cm wavelength
CloudSat
3 mm wavelength
JJAS DJF
Locations of the deepest and most intense convective cores seen by TRMM over ~14 years in South Asia and South America warm seasons
Near the large mountain ranges
Romatschke et al. 2010 Romatschke and Houze 2010
Relationship to Mountain Ranges and Moisture Sources
?
Andes
HimalayasRockies
How similar are the storms in these three regimes?
The North American Case
Carlson et al. 1983
moist
Texas
dry,hot
MexicanPlateau
Gulf ofMexico
Something similar happens to extreme convective cores in the
western region of South Asia
Sawyer 1947
A case observed by TRMM
TRMM PR Observations WRF Simulation
Medina et al. 2010
Consistent with Sawyer 1947
Consistent with Sawyer
1947
Backward trajectories (HYSPLIT/NCEP)
2.5 km
1.0 km
Medina et al. 2010
Consistent with Sawyer 1947
WRF Model Simulation
Mixing ratio CAPE
Medina et al. 2010
Surface wind
Medina et al. 2010
WRF Simulation
Cloud just after convection formed in the model
Triggering is over foothills—consistent with satellite data
A similarregime occurs near the Andes
Convective Regimes in South AmericaIdentified by TRMM
Romatschke and Houze 2010
Example of triggering over
the Sierra Cordóba range
Rasmussen & Houze 2011
What the storm looked
like on the TRMM radar
Rasmussen and Houze 2011
Vertical air motions
Low-level winds
COMPOSITEof average
conditions for storms with
intense convection
seen by the TRMM radar
downup
moistunstable
Rasmussen and Houze 2011
Recap
SIMILARITIES
• Channeling of moisture
• Downwind capping
• Explosive triggeringDIFFERENCES
• Capping may be downslope from a plateau or response to flow over a ridge
• Triggering may be meteorological or orographic
?Himalayas
Andes
Rockies
LARGE MOUNTAIN RANGES NEAR WARM MOIST ZONES
• Pakistan flood cases• Convection in the Madden-
Julian Oscillation• Storm systems over land and
ocean• Other…
Similar studies
The future
?Himalayas
Andes
Rockies
This research was supported by NASA grants NNX10AH70G, NNX10AM28G,
and NSF grant AGS1144105
TRMM
GPM
Next generation:
Radars need to be in the same orbit!
CloudSat EarthCare
End
?Himalayas
Andes
Rockies
This research was supported by NASA grants NNX10AH70G, NNX10AM28G,
and NSF grant AGS1144105
End
?Himalayas
Andes
Rockies
This research was supported by NASA grants NNX10AH70G, NNX10AM28G,
and NSF grant AGS1144105
Global Pattern of Deep Convection seen by TRMM
Zipser et al. 2006
Maximum height of TRMM’s most intense radar echoes