precipitation in the mediterranean region observed with trmm microwave data
DESCRIPTION
Precipitation in the Mediterranean region observed with TRMM microwave data. Martina Kästner & Jörg Steinwagner German Aerospace Center Applied Remote Sensing Cluster Oberpfaffenhofen, Germany. TRMM (Dec. 1997 – present) – NASA, NASDA. TRMM - Tropical Rainfall Measuring Mission. PR - PowerPoint PPT PresentationTRANSCRIPT
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Precipitation in the Mediterranean region observed with TRMM microwave data
Martina Kästner & Jörg Steinwagner
German Aerospace Center
Applied Remote Sensing Cluster
Oberpfaffenhofen, Germany
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M. Kästner, The 2004 EUMETSAT Meteorological Satellite Conference, Prague, Czech Republic, 2 June 2004
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TRMM - Tropical Rainfall Measuring Mission
TRMM (Dec. 1997 – present) – NASA, NASDA
PRPrecipitation Radar
TMITRMM microwaveImager
VIRSVisible infrared Scanner
CERESClouds and Earth‘sRadiant system
LISLightning imagingsensor
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TRMM
TRMM = Tropical Rainfall Measuring Mission
orbit in 400 km altitude
inclination 35°
PR = precipitation radar TMI = TRMM Microwave Imager
Frequency 13.8 GHz 10.7, 19.4, 21.3, 37.0, 85.5 GHz
Swath 250 km 880 km Horiz. resolution 5 km 5 to 70 km Vert. resolution 250 m Sensitivity 0.7 mm/h
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TRMM TMI brightness temperatures
Spain
North Africa
19 h
19 v
85 v
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Synoptic situation on 10 Nov 2001
trough > cut-off low > cyclogenesis
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common area: 15W ... 20E, 30N ... 60Ncommon grid, common period, common format
40°
60°
50°
40°
30°
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Retrieval 1 yes no
yes hits misses
no false correctalarms negativesO
bser
ved
Retrieval 1 Retrieval 2
Falsealarms
Hits
Misses
Correct negatives
categorical statistics
contingency table
Ret
rieva
l 2
accuracy, bias sc., false alarm rate, probability of detection, threat sc., equivalent threat sc., Hansen-Kuipers- , Heidke skill score
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Intercomparisons
rain gauge
PMW
IR
combined MW/IR
mesoscale model
neural network
radar
common grid (~28 km): ¼ deg lat x ¼ deg lon
PMW vs. PMW
PMW vs. combined MW/IR
PMW vs. BOLAM
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Intercomparison: PMW vs. PMW - different retrievals
visual inspection - subjective - all shown gridded precips are from 10 Nov. 2001, 03 UTCshown statistics are from all data (08 to 12 Nov. 2001)
FDA_bham (TMI) (Ch. Kidd, 1998)frequency differencealgorithm
Spain
North Africa
PATER (P. Bauer, 2001)PR Adjusted TMI Estimation of Rainfall
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statistics (8-12 Nov 2001)
N = 3.353 PATER PATERrain no rain
FDA rain 84 297FDA no rain 299 2673
accuracy = 0.82bias score = 1.00
PATER
FD
A
similar quality, PATER-RR tend to higher valuesstatistics driven by correct negatives
PMW vs. PMW
the best example
PATER
FD
A
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Combined (MW+IR) vs. PMW
MW + IR combined(J. Turk)
MW : PATER (P. Bauer)
MW : FDA_bham (Ch. Kidd)
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M. Kästner, The 2004 EUMETSAT Meteorological Satellite Conference, Prague, Czech Republic, 2 June 2004
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model BOLAM vs. PMW
MWBOLAM(A. Buzzi)
MW : PATER (P. Bauer)
MW : FDA_bham (Ch. Kidd)
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M. Kästner, The 2004 EUMETSAT Meteorological Satellite Conference, Prague, Czech Republic, 2 June 2004
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retrieval 1 retrieval 2
Falsealarms
Hits
Misses
Correct negatives
categorical statistics
N = 67 834
hits = 9 %misses = 15 %false alarms = 14 %corr. negatives = 62 %
accuracy = 0.71bias sc. = 0.96far = 0.61pod = 0.38ts = 0.24ets = 0.11hk = 0.19hss = 0.71
summary of all intercomparisons 0.25° grid
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Application: monthly mean precipitation
Nov 2002
Jan 2003
Mar 2003
May 2003
PATER algorithm(PMW)0.25° resolution~ 28 km
0 20 40 60 80 100 mm/month
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Conclusion
Over the Mediterranean heavy rainfall events occur several times a year
Need of improved weather forecasting of heavy rainfall
Need of rainfall data from over the sea -> satellites
Intercomparison of different satellite rainfall algorithms incl. model data,common grid = 0.25° (~28 km)
PMW techniques are directly related to 3-D structure of hydrometeors, but low revisit time; performance better over oceans than over land
IR techniques are widely used, but the physical relation of cloud top temperature and rain rate is weak; advantage: high revisit time
Combined techniques PMW and IR – TRMM 3B42, Turk, PERSIANN, etc.
Application of PATER PMW satellite rain retrieval:winter rain over the southern Mediterranean Seaand adjacent North Atlantic in high spatial resolution;seasonal changes in monthly mean precipitation
Step towards highly resolved precip climatology over sea
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M. Kästner, The 2004 EUMETSAT Meteorological Satellite Conference, Prague, Czech Republic, 2 June 2004
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M. Kästner, The 2004 EUMETSAT Meteorological Satellite Conference, Prague, Czech Republic, 2 June 2004
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RR comparison - 1DD – 9-13 November 2001
r = 0.71n = 146
Results
Bauer approach PATERPR + TMI (AMW + PMW)
Validation with 1DD GPCC data:r = 0.71 (n=146)
Assessment: PIP-3 (Adler, 2002)best: r = 0.75
FAR – min detectable RR for PATER:17 mm/d = 0.7 mm/h = 0.05 g/m³ lwc
Outlook
Combination IR +MWbetter cloud models