Monitoring the Quality of Operational and Semi-Operational Satellite Precipitation Estimates – The IPWG Validation / Intercomparison Study Beth Ebert Bureau.

Slides:



Advertisements
Similar presentations
Validation of Satellite Rainfall Estimates over the Mid-latitudes Chris Kidd University of Birmingham, UK.
Advertisements

Precipitation in IGWCO The objectives of IGWCO require time series of accurate gridded precipitation fields with fine spatial and temporal resolution for.
Quantification of Spatially Distributed Errors of Precipitation Rates and Types from the TRMM Precipitation Radar 2A25 (the latest successive V6 and V7)
Empirical Analysis and Statistical Modeling of Errors in Satellite Precipitation Sensors Yudong Tian, Ling Tang, Robert Adler, and Xin Lin University of.
Validation of Satellite Precipitation Estimates for Weather and Hydrological Applications Beth Ebert BMRC, Melbourne, Australia 3 rd IPWG Workshop / 3.
Gridded OCF Probabilistic Forecasting For Australia For more information please contact © Commonwealth of Australia 2011 Shaun Cooper.
Assessment of Tropical Rainfall Potential (TRaP) forecasts during the Australian tropical cyclone season Beth Ebert BMRC, Melbourne, Australia.
Validation of the Ensemble Tropical Rainfall Potential (eTRaP) for Landfalling Tropical Cyclones Elizabeth E. Ebert Centre for Australian Weather and Climate.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Quantitative precipitation forecasts in the Alps – first.
Phil Arkin, Earth System Science Interdisciplinary Center University of Maryland, College Park (Presenter) J. Janowiak, M. Sapiano, D. Vila, ESSIC/UMCP.
How low can you go? Retrieval of light precipitation in mid-latitudes Chris Kidd School of Geography, Earth and Environmental Science The University of.
The IPWG* Precipitation Validation Program The IPWG* Precipitation Validation Program Phillip A. Arkin and John Janowiak ESSIC/University of MarylandINTRODUCTION.
A Kalman Filter Approach to Blend Various Satellite Rainfall Estimates in CMORPH Robert Joyce NOAA/NCEP/CPC Wyle Information Systems Pingping Xie NOAA/NCEP/CPC.
1 GOES-R AWG Hydrology Algorithm Team: Rainfall Probability June 14, 2011 Presented By: Bob Kuligowski NOAA/NESDIS/STAR.
The Evaluation of a Passive Microwave-Based Satellite Rainfall Estimation Algorithm with an IR-Based Algorithm at Short time Scales Robert Joyce RS Information.
2 nd International IPWG Workshop Monterey, CA, October, 2004 The International Precipitation Working Group Arnold Gruber – NOAA/NESDIS, Camp Springs,
John Janowiak Climate Prediction Center/NCEP/NWS Jianyin Liang China Meteorological Agency Pingping Xie Climate Prediction Center/NCEP/NWS Robert Joyce.
Simultaneous Presence of 30 and 60 days ISO modes in Indian Summer Monsoon Observed from TRMM Merged Rainfall Data M S Narayanan National Atmospheric Research.
Verifying Satellite Precipitation Estimates for Weather and Hydrological Applications Beth Ebert Bureau of Meteorology Research Centre Melbourne, Australia.
CPC Unified Gauge – Satellite Merged Precipitation Analysis for Improved Monitoring and Assessments of Global Climate Pingping Xie, Soo-Hyun Yoo,
IPWG Validation current status and future directions Chris Kidd Beth Ebert John Janowiak The University of Birmingham, Birmingham, UK Bureau of Meteorology,
1 GOES-R AWG Hydrology Algorithm Team: Rainfall Potential June 14, 2011 Presented By: Bob Kuligowski NOAA/NESDIS/STAR.
Towards an object-oriented assessment of high resolution precipitation forecasts Janice L. Bytheway CIRA Council and Fellows Meeting May 6, 2015.
Fine-scale comparisons of satellite estimates Chris Kidd School of Geography, Earth and Environmental Sciences University of Birmingham.
Development and evaluation of Passive Microwave SWE retrieval equations for mountainous area Naoki Mizukami.
Improving Ensemble QPF in NMC Dr. Dai Kan National Meteorological Center of China (NMC) International Training Course for Weather Forecasters 11/1, 2012,
Latest results in verification over Poland Katarzyna Starosta, Joanna Linkowska Institute of Meteorology and Water Management, Warsaw 9th COSMO General.
Combining CMORPH with Gauge Analysis over
1 Program to Evaluate High Resolution Precipitation Products (PEHRPP): An Update Matt Sapiano P. Arkin, J. Janowiak, D. Vila, Univ. of Maryland/ESSIC,
VALIDATION AND IMPROVEMENT OF THE GOES-R RAINFALL RATE ALGORITHM Background Robert J. Kuligowski, Center for Satellite Applications and Research, NOAA/NESDIS,
Evaluation of Passive Microwave Rainfall Estimates Using TRMM PR and Ground Measurements as References Xin Lin and Arthur Y. Hou NASA Goddard Space Flight.
Verification of Precipitation Areas Beth Ebert Bureau of Meteorology Research Centre Melbourne, Australia
Validation of Satellite-Derived Rainfall Estimates and Numerical Model Forecasts of Precipitation over the US John Janowiak Climate Prediction Center/NCEP/NWS.
Evaluation of gridded multi-satellite precipitation (TRMM -TMPA) estimates for performance in the Upper Indus Basin (UIB) Asim J Khan Advisor: Prof. Dr.
TRMM TMI Rainfall Retrieval Algorithm C. Kummerow Colorado State University 2nd IPWG Meeting Monterey, CA. 25 Oct Towards a parametric algorithm.
1 Validation for CRR (PGE05) NWC SAF PAR Workshop October 2005 Madrid, Spain A. Rodríguez.
An Overview of Satellite Rainfall Estimation for Flash Flood Monitoring Timothy Love NOAA Climate Prediction Center with USAID- FEWS-NET, MFEWS, AFN Presented.
The Potential Role of the GPM in Activities at the Naval Research Laboratory Joe Turk and Jeff Hawkins Naval Research Laboratory Marine Meteorology Division.
WRF Verification Toolkit Workshop, Boulder, February 2007 Spatial verification of NWP model fields Beth Ebert BMRC, Australia.
1 GOES-R AWG Product Validation Tool Development Hydrology Application Team Bob Kuligowski (STAR)
Diurnal Cycle of Precipitation Based on CMORPH Vernon E. Kousky, John E. Janowiak and Robert Joyce Climate Prediction Center, NOAA.
1 Application of MET for the Verification of the NWP Cloud and Precipitation Products using A-Train Satellite Observations Paul A. Kucera, Courtney Weeks,
11 Short-Range QPF for Flash Flood Prediction and Small Basin Forecasts Prediction Forecasts David Kitzmiller, Yu Zhang, Wanru Wu, Shaorong Wu, Feng Ding.
VALIDATION OF HIGH RESOLUTION SATELLITE-DERIVED RAINFALL ESTIMATES AND OPERATIONAL MESOSCALE MODELS FORECASTS OF PRECIPITATION OVER SOUTHERN EUROPE 1st.
Evaluation of Precipitation from Weather Prediction Models, Satellites and Radars Charles Lin Department of Atmospheric and Oceanic Sciences McGill University,
A Physically-based Rainfall Rate Algorithm for the Global Precipitation Mission Kevin Garrett 1, Leslie Moy 1, Flavio Iturbide-Sanchez 1, and Sid-Ahmed.
Application of Probability Density Function - Optimal Interpolation in Hourly Gauge-Satellite Merged Precipitation Analysis over China Yan Shen, Yang Pan,
Dec 12, 2008F. Iturbide-Sanchez Review of MiRS Rainfall Rate Performances F. Iturbide-Sanchez, K. Garrett, S.-A. Boukabara, and W. Chen.
National Aeronautics and Space Administration Jet Propulsion Laboratory California Institute of Technology Pasadena, California
Validation of Satellite Rainfall Estimates over the Mid-latitudes Chris Kidd University of Birmingham, UK.
A Prototype Algorithm for Gauge – Satellite Merged Analysis of Daily Precipitation over Land
*CPC Morphing Technique
PEHRPP Geneva, 3-5 December 2007
Systematic timing errors in km-scale NWP precipitation forecasts
Verifying Precipitation Events Using Composite Statistics
Multi-scale validation of high resolution precipitation products
National Science and Technology Center for Disaster Reduction /
Radar/Surface Quantitative Precipitation Estimation
Requirements for microwave inter-calibration
Peter May and Beth Ebert CAWCR Bureau of Meteorology Australia
Zhong Liu1,2, Dana Ostrenga1,3, William Teng1,4, and Steven Kempler1
Soo-Hyun Yoo and Pingping Xie
Welcome to The Third Workshop of the
Rain Gauge Data Merged with CMORPH* Yields: RMORPH
Validation of Satellite Precipitation Estimates using High-Resolution Surface Rainfall Observations in West Africa Paul A. Kucera and Andrew J. Newman.
Satellite Foundational Course for JPSS (SatFC-J)
NOAA Objective Sea Surface Salinity Analysis P. Xie, Y. Xue, and A
6th IPWG Workshop October 2012, Sao Jose dos Campos, Brazil
An Inter-comparison of 5 HRPPs with 3-Hourly Gauge Estimates
Presentation transcript:

Monitoring the Quality of Operational and Semi-Operational Satellite Precipitation Estimates – The IPWG Validation / Intercomparison Study Beth Ebert Bureau of Meteorology Research Center Melbourne, Australia 2 nd IPWG Meeting, Monterey, October 2004

Motivation – provide information to...  Me...! fill the blank spot  Algorithm developers How well is my algorithm performing? Where/when is it having difficulties? How does it compare to the other guys?  Climate researchers Do the satellite rainfall products give the correct rain amount by region, season, etc?  Hydrologists Are the estimated rain volumes correct?  NWP modelers Do the satellite products put the precipitation in the right place? Is it the right type of precipitation?  Forecasters and emergency managers Are the timing, location, and maximum intensities correct?

Web page for Australia – home

Earlier studies GPCP Algorithm Intercomparison Programs (AIPs) and WetNet Precipitation Intercomparison Programs (PIPs) found:  Performance varied with sensor Passive microwave estimates more accurate than IR and VIS/IR estimates for instantaneous rain rates IR and VIS/IR slightly more accurate for daily and monthly rainfall due to better space/time sampling  Performance varied with region and season Tropics better than mid- and high latitudes Summer better than winter (convective better than stratiform)  Model reanalyses performed poorer than satellite algorithms for monthly rainfall in tropics, but competitively in mid-latitudes (PIP-3)

More recent studies  Combination of microwave and IR gives further improvement at all time scales Good accuracy of microwave rain rates Good space/time sampling from IR (geostationary)  Strategies Weighted combination of estimates Using match-ups of microwave and geostationary estimates  Get a field of multiplicative correction factors  Tune parameters of IR algorithm  Map IR T B onto microwave rain rates Morphing of successive microwave estimates using time evolution from geostationary imagery  Paradigm for GPM?

Focus of IPWG validation / intercomparison study 1. Updated evaluation of satellite rainfall algorithms

Quantitative Precipitation Forecasts (QPFs) from Numerical Weather Prediction (NWP)  WCRP Working Group on Numerical Experimentation (WGNE) has been validating / intercomparing model QPFs since 1995  Results Performance varies with region and season  Mid-latitudes better than tropics  Winter better than summer (stratiform better than convective) NWP performance is complementary to satellite performance! NWP performance over Germany

Foci of IPWG validation / intercomparison study 1. Updated evaluation of satellite rainfall algorithms 2. Where, when, under which circumstances is NWP rainfall better than satellite rainfall, and visa versa?

Related studies

Related studies O bserved P recipitation V alidation

Parameters of study  Evaluate estimates for at least one year to get seasonal variations in performance  As many different regions (climate regimes) as possible So far:  Australia  United States  Western Europe  Any volunteers for Asia? Elsewhere?  Focus on daily rainfall  Rain gauge and radar rainfall analyses used as reference data  Focus on relative accuracy  Global estimates archived at U. Maryland

Algorithms  Operational and semi-operational algorithms Run every day Available to public via web or FTP Experimental algorithms OK  Sorted by sensor type Microwave IR or VIS/IR Microwave + IR  Blending strategy NWP models  Global models (ECMWF, US) Lower spatial resolution, global coverage  Regional models Higher spatial resolution, limited coverage

Evaluation methodology  Daily rainfall estimates of Rain occurrence Rain amount  Spatial resolution Finest possible resolution (typically 0.25° lat/lon) Coarser resolution (1° lat/lon) for comparison with NWP  Stratify by Season Region Algorithm type  Algorithm Rain amount threshold

Verification methods  Rain occurrence Frequency bias Probability of detection and false alarm ratio Equitable threat score  Rain amount Multiplicative bias RMS error Correlation coefficient Probability of exceedance  Properties of rain systems Contiguous Rain Area (CRA) validation method (Ebert and McBride, 2000)  Rain area, volume, maximum amount  Spatial correlation  Error decomposition into volume vs. pattern

Some results for Australia...

User page  Targeted to external users of satellite rainfall products

Developer page  Targeted to algorithm developers – contains more algorithms, some of which aren't publicly available (at least not easily)

Multi-algorithm maps  All algorithms and NWP models for 30 September 2004 over Australia

Basic daily validation product  Maps and statistics

Daily CRA validation  Properties of rain system Area Mean and maximum rain accumulation Rain volume Spatial correlation Error decomposition into volume and pattern error components

Monthly and seasonal summaries  Variety of statistical plots Time series Scatter plots Table of statistics Binary (categorical) scores as a function of rain threshold Error as a function of estimated (observed) rain rate

Intercomparison of algorithm types Australian Tropics Australian Mid-latitudes Multiplicative bias December September ° grid summer autumn winter spring

Intercomparison of algorithms Australian Tropics Australian Mid-latitudes POD December September ° grid

Caveats  Reference data (gauge and radar analyses) are not as accurate as targeted ground validation sites Performance results more meaningful in a relative sense than in an absolute sense  No ocean validation Microwave algorithms are expected to have better performance over ocean because emission signal is used Therefore microwave+IR algorithms should also perform better over ocean NWP QPFs perform better over land than over ocean since more observations used in model initialization  Not all algorithms cover the same period (some missing data)

Future of this study  Results so far will be examined closely and written up for publication  Satellite precipitation validation / intercomparison will continue into the future...  Algorithm developers Keep making your results available Good opportunity to check new or updated algorithms  Reference data providers Thanks for data currently provided More is better! Can you assist in the validation itself?  Users of validation results Are we giving you the information you need? Please provide feedback and suggestions for improvement