Current Operational Data Capabilities, Issues and Perspectives Chandra Kondragunta Hydrometeorology Group Hydrology Laboratory Office of Hydrologic Development.

Slides:



Advertisements
Similar presentations
Surface Transportation Weather Research Center University of North Dakota Pavement Precipitation Accumulation Precipitation Data Sources Presenter: Mark.
Advertisements

Multiple Sensor Precipitation Estimation over Complex Terrain AGENDA I. Paperwork A. Committee member signatures B. Advisory conference requirements II.
Usage of Satellite Precipitation Estimates by HAS Forecasters at the West Gulf RFC Usage of Satellite Precipitation Estimates by HAS Forecasters at the.
Analysis of Radar-Rain Rate Relations During the Southeast Texas Flood Event of 18 April 2009 Steve Vasiloff, NOAA/National Severe Storms Laboratory Jeffrey.
Quantification of Spatially Distributed Errors of Precipitation Rates and Types from the TRMM Precipitation Radar 2A25 (the latest successive V6 and V7)
Site Specific Headwater Predictor National Weather Service 1 SSHP (Site Specific Headwater Predictor) How to Better use SSHP ER Flash Flood Workshop June.
Calibration of GOES-R ABI cloud products and TRMM/GPM observations to ground-based radar rainfall estimates for the MRMS system – Status and future plans.
Generating Quantitative Precipitation Forecasts for River Modeling
Radar-Derived Rainfall Estimation Presented by D.-J. Seo 1 Hydrologic Science and Modeling Branch Hydrology Laboratory National Weather Service Presented.
Rainfall Monitioring Using Dual-polarization Radars Alexander Ryzhkov National Severe Storms Laboratory / University of Oklahoma, USA.
Satellite Rainfall Estimation Robert J. Kuligowski NOAA/NESDIS/STAR 3 October 2011 Workshop on Regional Flash Flood Guidance System—South America Santiago.
Scott Kroeber RGIS – Great Plains Regional Weather Information Center
Temperature and Precipitation Data CBRFC Stakeholder Forum July 31, 2012.
Detection of Heavy Precipitation OHD’s Research and Development in Radar and Multisensor Applications David Kitzmiller Hydrologic Science and Modeling.
Automated Real-Time Operational Rain Gauge Quality-Control Tools in NWS Hydrologic Operations Chandra R. Kondragunta 1 and Kiran Shrestha 2 1 Hydrology.
Aaron Reynolds WFO Buffalo.  All NWS radars have dual polarization capability.  Dual Pol Expectations:  Ability to determine Precip type.  More info.
March 14, 2006Intl FFF Workshop, Costa Rica Weather Decision Technologies, Inc. Hydro-Meteorological Decision Support System Bill Conway, Vice President.
49 COMET Hydrometeorology 00-1 Matt Kelsch Tuesday, 19 October 1999 Radar-Derived Precipitation Part 3 I.Radar Representation of.
1 GOES-R AWG Hydrology Algorithm Team: Rainfall Probability June 14, 2011 Presented By: Bob Kuligowski NOAA/NESDIS/STAR.
Integration of Multiple Precipitation Estimates for Flash Flood Forecasting Reggina Cabrera NOAA/National Weather Service.
Comparison of PPS and QPE Rainfall Estimates for Summer 2013 Heavy Precipitation Events Comparison of PPS and QPE Rainfall Estimates for Summer 2013 Heavy.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Science Support for NASA-NOAA Research to Operations (R2O) and GPM Ralph.
What Affects Forecast Quality Uncertainty in weather forecasts Data Network density Quality of measurements Missing measurements Loss of data sites used.
NREPS Applications for Water Supply and Management in California and Tennessee. Patrick Gatlin 1, Mariana Felix Scott 1, Lawrence D. Carey 1, and Walter.
Wayne Faas Chief, NOAA National Climatic Data Center Data Operations Division December 3, 2003.
Anthony DeAngelis. Abstract Estimation of precipitation provides useful climatological data for researchers; as well as invaluable guidance for forecasters.
Center for Hydrometeorology and Remote Sensing, University of California, Irvine Basin Scale Precipitation Data Merging Using Markov Chain Monte Carlo.
Fine-scale comparisons of satellite estimates Chris Kidd School of Geography, Earth and Environmental Sciences University of Birmingham.
COMET HYDROMET Enhancements to PPS Build 10 (Nov. 1998) –Terrain Following Hybrid Scan –Graphical Hybrid Scan –Adaptable parameters appended to.
Multi-Sensor Precipitation Estimation Presented by D.-J. Seo 1 Hydrologic Science and Modeling Branch Hydrology Laboratory National Weather Service Presented.
Robert Hartman Acting Director NWS Office of Hydrologic Development GPM in the NOAA Integrated Water Forecasting Program.
Gridded Rainfall Estimation for Distributed Modeling in Western Mountainous Areas 1. Introduction Estimation of precipitation in mountainous areas continues.
Overview of the Colorado Basin River Forecast Center Lisa Holts.
Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN) Kuolin Hsu, Yang Hong, Dan Braithwaite, Xiaogang.
Operational Issues from NCDC Perspective Steve Del Greco, Brian Nelson, Dongsoo Kim NOAA/NESDIS/NCDC Dongjun Seo – NOAA/NWS/OHD 1 st Q2 Workshop Archive,
NEXRAD Data and Products at NCDC
VALIDATION OF HIGH RESOLUTION PRECIPITATION PRODUCTS IN THE SOUTH OF BRAZIL WITH A DENSE GAUGE NETWORK AND WEATHER RADARS – FIRST RESULTS Cesar Beneti,
Real-time Verification of Operational Precipitation Forecasts using Hourly Gauge Data Andrew Loughe Judy Henderson Jennifer MahoneyEdward Tollerud Real-time.
The NOAA Hydrology Program and its requirements for GOES-R Pedro J. Restrepo Senior Scientist Office of Hydrologic Development NOAA’s National Weather.
Current and Future Data Requirements Chandra Kondragunta Hydrometeorology Group Hydrology Laboratory Office of Hydrologic Development NOAA/National Weather.
Distributed Hydrologic Modeling-- Jodi Eshelman Analysis of the Number of Rain Gages Required to Calibrate Radar Rainfall for the Illinois River Basin.
July 31, 2012 Kevin Werner NWS Colorado Basin River Forecast Center Tim Bardsley Western Water Assessment 1 Future Colorado Basin Observing System.
Multi-Radar, Multi-Sensor: A Successful Case of Research-To-Operations
CPC Unified Precipitation Project Pingping Xie, Wei Shi, Mingyue Chen and Sid Katz NOAA’s Climate Prediction Center
Evaluation of Passive Microwave Rainfall Estimates Using TRMM PR and Ground Measurements as References Xin Lin and Arthur Y. Hou NASA Goddard Space Flight.
6/29/2005 Q2 Workshop, Norman, OK 3-D Radar Mosaic and Initial Q2 Development Plans Jian Zhang 1, Ken Howard 2, and Steve Vasiloff 2 1 University of Oklahoma,
Flash Flood Monitoring and Prediction Current Operational Capabilities, Issues and Perspectives Britt Westergard, Service Hydrologist WFO Jackson, KY Q2.
1 National HIC/RH/HQ Meeting ● January 27, 2006 version: FOCUSFOCUS FOCUSFOCUS FOCUS FOCUSFOCUS FOCUSFOCUS FOCUSFOCUS FOCUSFOCUS FOCUSFOCUS FOCUSFOCUS.
Travis Smith Hazardous Weather Forecasts & Warnings Nowcasting Applications.
Alexander Ryzhkov Weather Radar Research Meteorological Applications of Dual-polarization Radar.
1 NOHRSC Challenges of using Snow Data Carrie Olheiser Office of Hydrologic Development National Weather Service, NOAA U.S. Department of Commerce National.
WSR-88D PRECIPITATION ESTIMATION FOR HYDROLOGIC APPLICATIONS DENNIS A. MILLER.
Flash Flood Prediction Working Group Q2 Workshop June 28-30, 2005.
Asia Flood Network— A USAID Program for Flood Mitigation and Preparedness in Asia Asia Flood Network Program Objective –Identify and fill gaps in end-to-end.
MPE Software Upgrades for Dual Pol Radars MPE Software Upgrades for Dual Pol Radars Sep 19, Edward Clark, Paul Tilles, David Kitzmiller Mark Fenbers,
Research To Operations For Improved Precipitation Estimates and Forecasts David Kitzmiller Group Leader - Hydrometeorology Hydrology Laboratory, Office.
1 GOES-R AWG Product Validation Tool Development Hydrology Application Team Bob Kuligowski (STAR)
Ken Cook – SOO NWS Wichita, KS (ICT) An Assessment of Using the Mean Field Bias Correction to Improve Precipitation Estimates Ken Cook and Maggie Schoonover.
Overview of CBRFC Flood Operations Arizona WFOs – May 19, 2011 Kevin Werner, SCH.
11 Short-Range QPF for Flash Flood Prediction and Small Basin Forecasts Prediction Forecasts David Kitzmiller, Yu Zhang, Wanru Wu, Shaorong Wu, Feng Ding.
Estimating Rainfall in Arizona - A Brief Overview of the WSR-88D Precipitation Processing Subsystem Jonathan J. Gourley National Severe Storms Laboratory.
AN IMPROVED USER INTERFACE FOR VIEWING NWS HOURLY PRECIPITATION GRAPHICS NATIONAL FLOOD WORKSHOP OCT 26, 2010 Bill Lawrence Service Coordination Hydrologist.
NWS Precipitation Analysis Product Victor Murphy NWS Southern Region Climate Service Program Mgr. 5 th US Drought Monitor Forum Portland, OR October 11,
“CMORPH” is a method that creates spatially & temporally complete information using existing precipitation products that are derived from passive microwave.
Travis Smith U. Of Oklahoma & National Severe Storms Laboratory Severe Convection and Climate Workshop 14 Mar 2013 The Multi-Year Reanalysis of Remotely.
Estimation of precipitation over the OLYMPEX domain during winter
Multi-Sensor Precipitation Estimation
Radar/Surface Quantitative Precipitation Estimation
Validation of Satellite Precipitation Estimates using High-Resolution Surface Rainfall Observations in West Africa Paul A. Kucera and Andrew J. Newman.
Monitoring for Flood and Water Supply Forecasting
Presentation transcript:

Current Operational Data Capabilities, Issues and Perspectives Chandra Kondragunta Hydrometeorology Group Hydrology Laboratory Office of Hydrologic Development NOAA/National Weather Service Q2 Workshop Norman, OK June 28, 2005

Outline. QPE requirements for NWS operations. Current operational data capabilities and issues. Potential other data sets for QPE. Field perspectives. Summary

QPE Requirements Priority Category : “1” = Mission Critical : Cannot meet operational mission objectives without this data set Priority Category : “1” = Mission Critical : Cannot meet operational mission objectives without this data set Threshold Objective Threshold Objective Spatial Res. 1 km 0.5km Spatial Res. 1 km 0.5km Temporal Res. 6 min. 1 min. Temporal Res. 6 min. 1 min. Accuracy 1 mm/hour 0.25 mm/hour Accuracy 1 mm/hour 0.25 mm/hour Data Latency 3 min. 1 min. Data Latency 3 min. 1 min. Mapping Accuracy 0.2 km 0.1 km Mapping Accuracy 0.2 km 0.1 km

Current operational data capabilities and issues

Data Sources Current sources of data for QPE in NWS: 1. Rain gauge data 1. Rain gauge data 2. WSR-88D radar rainfall estimates 2. WSR-88D radar rainfall estimates 3. Satellite Precipitation Estimates 3. Satellite Precipitation Estimates 4. NWP model output 4. NWP model output

Rain Gauge Data Rain gauge data for NWS operations come from several different sources: HADS:. Federal & State Wildland Fire Programs --- 2,400 rain gages. USGS --- 1,734 rain gages. USACE --- 1,637 rain gages. NWS rain gages. 117 other DCS Platform operators (USBR, TVA etc.) Other:. S tate and local government funded agencies (Mesonets). Automated Surface Observing System. Cooperative rain gauge network. Other NWS supported gauges (IFLOWS, ALERT etc.) Spatial resolution : Non-uniform Temporal resolution : hourly and daily (few 1 min. gauges)

HADS Hydrometeorological Automated Data System:. An integrator of in situ data. Acquires non-standard raw data relayed via GOES Data Collection System (DCS). More than 1.7 million observational values processed each day. 11,500 data reporting locations. 97% of data network is non-NOAA. A future component of NOAA’s Integrated Surface Observing System (ISOS) Program

Issues with rain gauge data There are several issues with rain gauge data: Coverage : Uneven spatial and temporal coverage, Sparse network density for some regions Quality : Gauge data quality is a big problem Examples: Transmission errors, staggered reporting times, frozen gauges, outliers, missing data etc Timeliness : Reports arriving late Errors:. Wind effects --- Under catch. Wind effects --- Under catch. Gauge exposure blockages (trees, buildings etc.) --- Under catch. Gauge exposure blockages (trees, buildings etc.) --- Under catch. Solid precipitation --- under catch. Solid precipitation --- under catch. Heavy rain rates --- under catch. Heavy rain rates --- under catch. Strong wind --- over catch. Strong wind --- over catch

Density is uneven and poor in Nevada

Radar Rainfall Estimates Current radar rainfall estimates come from WSR88D radar network Spatial resolution : 2km x 1 Deg. Spatial resolution : 2km x 1 Deg. Temporal resolution : 6 min. Temporal resolution : 6 min. Issues: Beam blockage, under estimation, over estimation, detection problem, Anomalous propagation etc.

Effective CNRFC Radar CoverageEffective NWRFC Radar Coverage

Satellite Precipitation Estimates Current Satellite Precipitation Estimates (SPE) come from GOES satellite. They are generated by an algorithm called the HydroEstimator. Spatial resolution : 4 km Spatial resolution : 4 km Temporal resolution : 15 min. Temporal resolution : 15 min. Issues: Under estimation, over estimation, detection problem, mis-location of precipitation

NWP output Several NWP model outputs such as RUC, MM5, MOS, NDFD etc. are used in operations Spatial resolution : 5 km Spatial resolution : 5 km Temporal resolution : 1 hr Temporal resolution : 1 hr Issue: Accuracy of model output

MPE Multi-sensor Precipitation Estimator (MPE) is an operational software currently being used at several NWS field offices to generate QPE. It uses rain gauge, radar and satellite precipitation estimates to generate multi-sensor QPE The main features of MPE are:. Delineation of effective radar coverage. Mosaicking based on radar sampling geometry. Service area-wide precipitation analysis. Mean field bias correction of radar rainfall estimates. Local bias correction of radar and satellite precipitation estimates. Semi-automated rain gauge QC tools. Several GUI tools to interactively modify the point values or gridded fields

ORPG/PPS RFC Multi-Sensor Precipitation Estimator (MPE) WSR-88DDPA Hydro-Estimator Rain Gauges Mean Field/local Bias correction MPE Local Bias correction

MEAN FIELD BIAS (MFB) ADJUSTMENT Before Correction After Correction

MULTISENSOR (GAUGE+RADAR) ESTIMATION FILLS MISSING AREAS Bias CorrectedMulti-sensor

Hydroestimator (mm)Local Bias-Corrected Hydroestimator CNRFC 24-Hour Precipitation, 17 Dec 2002

Gauge QC in MPE Spatial Consistency Check (semi-automated):. Checks for consistency of a gauge value with the neighboring gauge values in all four quadrants. Checks for consistency of a gauge value with the neighboring gauge values in all four quadrants. Lightning data is used to screen the gauges received rainfall from convective systems before flagging the outliers. Lightning data is used to screen the gauges received rainfall from convective systems before flagging the outliers Multi-Sensor Check (semi-automated):. Compares the rain gauge values with radar estimates and points out the stuck gauges Display 7X7:. Ability to display 7X7 HRAP bins centered on a gauge to aid manual gauge QC. Ability to display 7X7 HRAP bins centered on a gauge to aid manual gauge QC

Spatial Consistency Check

Multi-sensor check

Locally Grown Capabilities Some of the locally grown software are. Mountain Mapper : To generate gridded QPE, gauge QC (mostly in the western region). XNAV, XDAT to QC gauge data

Potential other data sets for QPE. Reflectivity data from the Terminal Doppler Weather Radar. Canadian radar data (NMQ). Microwave satellite precipitation estimates from SSM/I sensors. Precipitation estimates from the TRMM. Lightning data

Field Perspectives

Rain Gauge Data. “There are always issues with rain gauge data. Missing data, Zero reports, transmission errors, tipping bucket errors, poorly maintained equipment (particularly with IFLOWS) staggered reporting times etc.” --- OHRFC. “There are always issues with rain gauge data. Missing data, Zero reports, transmission errors, tipping bucket errors, poorly maintained equipment (particularly with IFLOWS) staggered reporting times etc.” --- OHRFC (Several other RFCs expressed similar view point) (Several other RFCs expressed similar view point). “High elevation data, such as SNOTEL has problems because of the freezing of the gauge” --- NWRFC. “ WGRFC has numerous gauge – sparse areas over roughly the western half of our region. Gauges are densely clustered in our largest cities due to ALERT systems. There can be issues with data quality and timeliness within these systems” --- WGRFC

Radar Data. “Over and under estimation, significant gaps in coverage, lack of coverage of basins in Canada, gross underestimation in winter, inconsistent Z/R relationships in adjoining radars” --- NCRFC. “Over and under estimation, significant gaps in coverage, lack of coverage of basins in Canada, gross underestimation in winter, inconsistent Z/R relationships in adjoining radars” --- NCRFC (Several RFC expressed similar view point) (Several RFC expressed similar view point). “ Radar data in our area is of no use in generating QPE. Beam blockage, inadequate coverage, melting level bright band etc.” --- CNRFC. “Radar is useless in the NWRFC area” --- NWRFC. “We use MPE and have the usual radar issue: under/over estimation of rainfall, radar coverage, bright banding …” LMRFC

Satellite Precipitation Estimates. “We don’t use satellite precipitation estimates because of poor quality” --- LMRFC. “We don’t use satellite precipitation estimates because of poor quality” --- LMRFC (Most of the RFCs expressed similar view point) (Most of the RFCs expressed similar view point). “ We use it EXTREMELY rarely, when there is no other data. Maybe 1 time in cases. It has proven to be of poor quality for the most part ” --- ABRFC. “WGRFC supplements the radar void regions with SPE.” --- WGRFC

Summary In summary,. Rain gauge data quality is an issue for current NWS hydrologic operations. Need to develop automated gauge QC techniques to satisfy the next generation QPE algorithm demands. Need to improve the rain gauge network density to improve the data coverage. Need to address the radar coverage gap issues by bringing in alternate data sets, such as satellite precipitation estimates and NWP model output. Need to address the radar rainfall estimation issues (over/under estimation)

Summary (Contd.). Need to improve the satellite precipitation quality by developing multi-platform, multi-sensor (IR+MW) techniques. Need to make better use of NWP model output in QPE estimation

Questions?

COOP network

Rain gauge in snow

Rain gauge site