TU2.L10 - NEXT-GENERATION GLOBAL PRECIPITATION PRODUCTS AND THEIR APPLICATIONS
- 1. Next-Generation Global Precipitation Products and Their Applications Arthur Y. Hou NASA Goddard Space Flight Center Session TU2.L10 IGARSS, 27-30 July 2010
- 2. Current Generation of Global Precipitation Products TRMM radar/radiometer system provided an anchor for rainfall estimates by passive microwave sensors in the tropics and subtropics. Further improvements will require better spaceborne sensors and inversion algorithms (especially for light rain and falling snow). Current multi-satellite products are based on MW or MW+IR observations from uncoordinated satellite missions using a variety of merging techniques 50N 50S TRMM Realtime 3hr global rain map at 0.25 o resolution
- 3. Accuracy of instantaneous precipitation estimate Spatial coverage & temporal sampling (for improved estimation of precipitation accumulation) Spatial resolution (for local-scale applications) Data latency (for near real-time operational use) An international satellite mission specifically designed to deliver “next-generation” precipitation observations from space for research and applications. Key to Better Global Precipitation Data Products: The Global Precipitation Measurement (GPM) Mission
- 4. GPM Mission Concept Key Contribution Refine constellation sensor retrievals within a consistent framework to provide next-generation global precipitation data products Partner Satellites: GCOM-W1 DMSP F-18, F-19/20 Megha-Tropiques MetOp, NOAA-19 NPP, JPSS (over land) Unify and advance global precipitation measurements from space using a constellation of research and operational microwave sensors GPM Core Observatory (65 o ) DPR (Ku-Ka band) GMI (10-183 GHz) (NASA-JAXA, LRD 2013) Precipitation physics observatory Transfer standard for inter-satellite calibration of constellation sensors Enhanced capability for ci near-realtime monitoring ci of hurricanes & ci midlatitude storms Improved accuracy in ci rain accumulation Low Inclination Observatory (40 o ) GMI (10-183 GHz) (NASA & Partner, 2014) Coverage & Sampling 1-2 hr revisit time over land < 3 hr mean revisit time over 90% of globe
- 5. NASA-JAXA GPM Core Observatory Increased sensitivity (~12 dBZ) for light rain and snow detection relative to TRMM Better measurement accuracy with differential attenuation correction Detailed microphysical information (DSD mean mass diameter & particle no. density) & identification of liquid, ice, and mixed-phase regions Dual-Frequency (Ku-Ka band) Precipitation Radar (DPR): Multi-Channel (10-183 GHz) GPM Microwave Imager (GMI): Higher spatial resolution (IFOV: 6-26 km) Improved light rain & snow detection Improved signals of solid precipitation over land (especially over snow-covered surfaces) 4-point calibration to serve as a radiometric reference for constellation radiometers Combined Radar-Radiometer Retrieval DPR & GMI together provide greater constraints on possible solutions to improve retrieval accuracy Observation-based a-priori cloud database for constellation radiometer retrievals Core Observatory Measurement Capabilities
- 6. Intercalibrated constellation radiometric data (with differences in center frequency, viewing geometry, and resolution reconciled). Converting observations of one satellite to virtual observations of another using non-Sun-synchronous satellite as a transfer standard International working group (NASA, NOAA, JAXA, CONAE, CMA, EUMETSAT, CNRS, GIST, & universities) in coordination with WMO/CGMS GSICS Unified precipitation retrievals using a common hydrometeor database constructed from combined DPR+GMI measurements GPM Core: Reference Standard for Constellation Radiometers GPM Next-Generation Precipitation Products Optimally matching observed T b with simulated T b from an a priori cloud database Simulated T b Observed T b TRMM uses a model-generated cloud database GPM uses a DPR/GMI-constrained database Prototype GPM Radiometer Retrieval Comparison of TRMM PR surface rain with TMI rain retrieval using an cloud database consistent with PR reflectivity and GMI multichannel radiances ( Kummerow et al., CSU)
- 7. GPM Ground Validation Three complementary approaches: Direct statistical validation (surface): - Leveraging off operational networks to identify and resolve first-order discrepancies between satellite and ground-based precipitation estimates Physical process validation (vertical column): - Cloud system and microphysical studies geared toward testing and refinement of physically-based retrieval algorithms Integrated hydrologic validation/applications (4-dimensional): - Identify space-time scales at which satellite precipitation data are useful to water budget studies and hydrological applications; characterization of model and observation errors Pre-launch algorithm development & post-launch product evaluation Refine algorithm assumptions & parameters - Characterize uncertainties in satellite retrievals & GV measurements “ Truth” is estimated through the convergence of satellite and ground-based estimates
- 8. GPM Joint Field Campaigns: Joint campaign with Brazil on warm rain retrieval over land in Alcântara, 3-24 March 2010 Light Precipitation Validation Experiment (LPVEx): CloudSat-GPM light rain in shallow melting layer situations in Helsinki, Finland, Sept-Oct 2010 Mid-Latitude Continental Convective Clouds Experiment (MC3E): NASA-DOE field campaign in central Oklahoma, Apr-May 2011 High-Latitude Cold-Season Snowfall Experiment: Joint campaign with Environment Canada on snowfall retrieval in Ontario, Canada, Jan-Feb 2012 Hydrological validation with NOAA HMT in 2013 (under development) International Science Collaboration 15 Active International Projects Joint field campaigns National networks and other ground assets (radar, gauges, etc.) Hydrological validation sites (streamflow gauges, etc.) Pre-CHUVA (2010) MC3E (2011) NASA-EC Snowfall (2012) LPVEx (2010)
- 9. Baseline Constellation Schedule Hour Current Capability: < 3h over 45% of globe GPM (2015): < 3h over 90% of globe GPM Constellation Sampling and Coverage 1-2 hr revisit time over land with inclusion of sounders Prime Life Extended Life GPM Core Launch
- 10. GPM Observations from Non-Sun-Synchronous Orbits Monthly Samples as a Function of the Time of the Day (1 o x 1 o Resolution) Near real-time observations from the GPM Core and LIO between overpasses by polar orbiters at fixed times of the day for: Intercalibration of polar- m orbiting sensors over wide m range of latitudes Near real-time monitoring of m hurricanes & midlatitude m storms Improved accuracy of rain m volume estimation Resolving diurnal variability m in rainfall climatology TRMM: 3652 “asynoptic” samples GPM Core+LIO: 6175 samples Core+LIO: 4298 samples
- 11. GMI Sensor Resolution AMPR (Aircraft) GMI (Core) AMSR-E TMI SSMIS Synthesized Brightness Temperatures (Courtesy of R. Hood) Comparison of GMI resolution with other radiometers GMI on the Core Observatory altitude of 407 km will offer the highest resolution radiometric imaging data.
- 12. GPM Dynamically-Downscaled High-Resolution Product Assimilate satellite precipitation data into cloud-resolving model to produce observation-constrained dynamically-balanced precipitation analysis at 1-2 km for hydrological applications GPM Observations Cloud Resolving Model Level-4 Precipitation Analysis Using CRM to downscale satellite precipitation observations Results from NASA-CSU prototype WRF ensemble data assimilation system assimilating AMSR-E Tb Zupanski et al. Background (3-h fcst) Analysis (Conv+AMSR-E) Observed Tb 89v Cross section of Erin (35N) in 89v GHz
- 13. IFOV intercalibrated Tb and rain products for GMI within 1 hour of data collection Merged constellation radiometer precipitation products at several latency levels: Precipitation estimates based on data collected within past 1 hr (fast but incomplete space coverage) Precipitation estimates based on data collected within past 2 hrs Precipitation estimates based on data collected within past 3 hour Precipitation estimates based on data collected within past 6 hours (globally complete) Merged products updated with more observations every hour Data Latency
- 15. Applications of Precipitation Data Products (1/3) Hurricane Tracking Numerical Weather Prediction Position Error in Nautical Miles Precipitation observations are in use at ECMWF, NCEP, JMA, and other NWP centers to improve weather forecasting. ECMWF Hurricane Charley track forecasts from analysis 2004081112 Cyclone disappeared in operational forecast without rain assimilation Rain Ass Courtesy of P. Bauer/ECMWF
- 16. Applications of Precipitation Data Products (2/3) Global Flood Monitoring Landslide Hazard Forecasts On-line real-time estimates of flood areas using satellite rainfall and a hydrological model updated globally, every 3 hrs at 0.25° resolution (http://trmm.gsfc.nasa.gov) Landslide forecast every 3 hrs based on surface topographic variability, land cover, soil type/texture, drainage density, and rainfall amount (Hong et al.) Estimated Water Depth from Hydrological Model 35mm 75mm >125mm 4 Nov 2009 06 GMT
- 17. Applications of Precipitation Data Products (3/3) Freshwater Resource Monitoring Crop Forecasting Water stress relative to population growth is a major concern around the world. As the primary source of freshwater, global precipitation data are key to improving freshwater resource monitoring and management on seasonal basis. Precipitation data are in use by the USAID/USDA Famine Early Warning System Network (USAID/FEWS-Net) for crop and weather assessment around the world. Deficits in Water Requirement Satisfaction Index match field reports of reduced yields Courtesy of G. Senay, USGS/EDC
- 18. Applied research is essential for developing and refining techniques to increase the benefits of precipitation observations in many application areas: NWP, data assimilation, and reanlaysis: Advanced assimilation methods to extract maximum information from precipitation data in the presence of forecast model errors Improved characterization of precipitation error properties Enabling More Effective Use of GPM Data in Applications Hydrological modeling & prediction: Identify time-space scales at which satellite rainfall data become useful to water budget studies and hydrological applications Characterize uncertainties in hydrologic models and propagation of uncertainties in input data into model forecasts Develop downscaling precipitation products for local-scale hydrological modeling and prediction Current satellite rainfall products have useful skills in river discharge prediction over areas > 10 4 sq. miles STDE, BIAS, and N-S in Daily Streamflow E. Wood et al.
- 19. GPM is an international satellite mission specifically designed to unify and advance precipitation measurements from a constellation of microwave sensors for scientific research and societal applications. GPM is in the implementation phase at NASA and JAXA Core Observatory Launch Readiness Date: 21 July 2013 NASA Precipitation Processing System is currently producing Prototype intercalibrated L1 products for TMI, SSMI, AMSR-E, SSMIS, & WindSat L3 merged global precipitation products using TMI, SSMI, AMSR-E, AMSU, & MetOp in near real-time for research & applications GPM next-generation global precipitation products will build on intercalibrated microwave radiances and unified physical retrievals using a common hydrometeor database consistent with combined radar/radiometer measurements. Ground validation is key to algorithm physics improvement. NASA is conducting a series of joint field campaigns with domestic and international partners to refine algorithm assumptions and parameters. Innovative applied research is key to increasing the benefits of precipitation data in many application areas. Summary
Editor's Notes
- #7: WMO Coordination Group for Meteorological Satellites (CGMS) Global Space-based Inter-Calibration System - GSICS)