AMBER/FFMP Overview COMET Basin Customization 02-03 06 August 2002 Robert S. Davis, Pittsburgh NWSWFO.

Slides:



Advertisements
Similar presentations
Application of the FEWS Stream Flow (SF) Model to the Limpopo Basin, Mozambique Final Report Tanya Hoogerwerf.
Advertisements

Brian McInerney Hydrologist National Weather Service Hydrologic Outlook April 2006.
FFMP Advanced: Eastern Region Flash Flood Conference, May 2010 A Review for Experienced Users Eastern Region Flash Flood Conference Tom Filiaggi May 2010.
The Areal Mean Basin Estimated Rainfall (AMBER) Program A Tool to Assist in Flash Flood Forecasting Ami Arthur Cooperative Institute for Mesoscale Meteorological.
1 AMBER Areal Mean Basin Estimated Rainfall COMET Faculty Course Robert S. Davis, Pittsburgh WFO.
1 AMBER Areal Mean Basin Estimated Rainfall COMAP Symposium 00-3 Robert S. Davis, Pittsburgh WFO Presented by Tom Filiaggi.
The Influence of Basin Size on Effective Flash Flood Guidance
Continuous Hydrologic Simulation of Johnson Creek Basin and Assuming Watershed Stationarity Rick Shimota, P.E. Hans Hadley, P.E., P.G. The Oregon Water.
ESTIMATING THE 100-YEAR FLOOD FORDECORAH USING THE RAINFALL EVENTS OF THE RIVER'S CATCHMENT By Kai TsurutaFaculty Advisor: Richard Bernatz Abstract:This.
Upper Brushy Creek Flood Study – Flood mapping and management Rainfall depths were derived using USGS SIR , Atlas of Depth Duration Frequency.
Distributed Hydrologic Model-Threshold Frequency (DHM-TF) Reggina Cabrera NOAA/National Weather Service Eastern Region
NWS Hydrologic Forecasting. Functions and relations 2 River Forecast Center WFO 1WFO 2WFO 3 Implementation, calibration and execution of river forecast.
Lecture ERS 482/682 (Fall 2002) Rainfall-runoff modeling ERS 482/682 Small Watershed Hydrology.
GIS Applications in Meteorology and Hydrology John S. Quinlan NWS Albany, NY.
NOAA’s NWS and the USGS: Partnering to Meet America’s Water Information Needs Dr. Thomas Graziano Acting Chief, Hydrologic Services Division Office of.
Idaho's Climate and Water Resource Forecast for the 2008 Water Year Sponsored by: The Climatic Impacts Group at the University of Washington and the.
A Distributed Flash Flood Forecasting Rainfall- Runoff Model Applied to Watersheds in the Northeast United States Michael Schaffner NOAA National Weather.
WHAT IS Z?  Radar reflectivity (dBZ)  Microwave energy reflects off objects (e.g. hydrometeors) and the return is reflectivity WHAT IS R?  Rainfall.
June 23, 2011 Kevin Werner NWS Colorado Basin River Forecast Center 1 NOAA / CBRFC Water forecasts and data in support of western water management.
6/3/2010 ER FFG Conference An Overview of Gridded Flash Flood Guidance; A Spatially Distributed Runoff and Threshold-Runoff Based Approach Erick Boehmler.
“Flood monitoring and mapping for Emergency Response in San Antonio-Texas” Part I by Silvana Alcoz Source photo Term.
FNR 402 – Forest Watershed Management
National Basin Delineation Project Team: Ken Howard Ami Arthur Gina Cox Dave Slayter Nathan Kuhnert Cooperative Institute for Mesoscale Meteorological.
KINEROS (KINematic runoff and EROSion model) Michael Schaffner Senior Service Hydrologist NOAA National Weather Service WFO Binghamton, NY Eastern Region.
AMBER/FFMP Overview COMET Basin Customization August 2002 Robert S. Davis, Pittsburgh NWSWFO.
AWIPS Localization Issues COMET Basin Customization Course Michael Mercer March 2003.
March 14, 2006Intl FFF Workshop, Costa Rica Weather Decision Technologies, Inc. Hydro-Meteorological Decision Support System Bill Conway, Vice President.
SCAN SCAN System for Convection Analysis and Nowcasting Operational Use Refresher Tom Filiaggi & Lingyan Xin
Flash Flood Monitoring and Prediction (FFMP) Flash Flood Monitoring and Prediction-Advanced (FFMPA) Reggina Cabrera NOAA/National Weather Service Eastern.
A Statistical-Distributed Hydrologic Model for Flash Flood Forecasting International Workshop on Flash Flood Forecasting March 13, 2006 Seann Reed 1, John.
Integration of Multiple Precipitation Estimates for Flash Flood Forecasting Reggina Cabrera NOAA/National Weather Service.
Statewide Map-based IDF Analysis Norman Gonsalves for Caltrans.
Comparison of PPS and QPE Rainfall Estimates for Summer 2013 Heavy Precipitation Events Comparison of PPS and QPE Rainfall Estimates for Summer 2013 Heavy.
FLASH FLOOD PREDICTION James McDonald 4/29/08. Introduction - Relevance  90% of all national disasters are weather and flood related  Central Texas.
NOAA’s National Weather Service Flood and Flash Flood Warning Program Michelle Schmidt Western Region Hydrology and Climate Services Division.
ROFFG Romania Flash Flood Guidance System. The Romania Flash Flood Guidance System is an adaptation of the HRC Flash Flood Guidance System used in various.
1 AMBER Areal Mean Basin Estimated Rainfall COMAP Flash Flood Course Robert S. Davis, Pittsburgh WFO.
1 The August 21, 2009 Chelsea, VT Flash Flood Case Study and Radar Considerations Eastern Region Flash Flood Conference June Greg Hanson WFO BTV.
National Weather Service - Southeast River Forecast Center Southeast River Forecast Center North Florida Visit July 17-20, 2006 Southeast River Forecast.
COMET HYDROMET Enhancements to PPS Build 10 (Nov. 1998) –Terrain Following Hybrid Scan –Graphical Hybrid Scan –Adaptable parameters appended to.
1 Flash Floods: Defining and Forecasting Matt Kelsch COMAP Symposium 02-1, 02-2 Heavy Precip/Flash Flood October 2001 Fort Collins,
Multi-Sensor Precipitation Estimation Presented by D.-J. Seo 1 Hydrologic Science and Modeling Branch Hydrology Laboratory National Weather Service Presented.
National Weather Service Products on the Internet Erik Heden Meteorologist NWS Weather Forecast Office Binghamton, NY Patti Wnek Service Coordination Hydrologist.
Overview of the Colorado Basin River Forecast Center Lisa Holts.
1 Flash Floods in the South-Central U.S.: What are They and How Can we Forecast Them? Matt Kelsch Thursday, 30 March 2000 UCAR Cooperative Program for.
Flash Flood Monitoring and Prediction (FFMP) John Ferree Warning Decision Training Branch Norman, OK John Ferree Warning Decision Training Branch Norman,
Pittsburgh Urban Flash Flood May 18, AMBER Time Display Interval 5-minute ABR: Used to compute ABR Rate and to display 2-hour accumulated ABR.5-minute.
Storm Based Warnings A New Direction in the Warning Process Add Name National Weather Service Add Office.
Flash Flood A rapid and extreme flow of high water into a normally dry area, or a rapid water level rise in a stream or creek above a predetermined flood.
National Basin Delineation Project Team: Ken Howard Ami Arthur Gina Cox Dave Slayter Nathan Kuhnert Cooperative Institute for Mesoscale Meteorological.
WMS Investigation: Travel Time Variability with Method, Area, and Slope Ryan Murdock May 1, 2001.
Flash Flood Monitoring and Prediction Current Operational Capabilities, Issues and Perspectives Britt Westergard, Service Hydrologist WFO Jackson, KY Q2.
Flash Flood Monitoring and Prediction (FFMP) John Ferree Warning Decision Training Branch Norman, OK John Ferree Warning Decision Training Branch Norman,
Introduction to GIS. What is GIS? Geographic Information System Geographic implies of or pertaining to the surface of the earth Information implies knowledge.
FFMP Advanced: 4 th Regional Severe Storms / Radar and Hydrology Conference Overview, August 2009 An Overview for 4 th Regional Severe Storms / Radar and.
AMBER Areal Mean Basin Estimated Rainfall COMAP Symposium Heavy Precipitation and Flash Floods Robert S. Davis, Pittsburgh WFO.
An ArcView GIS Application for Deriving Threshold Runoff Values to assist with Flash Flood Guidance Seann M. Reed Research Hydrologist NWS-HRL Silver Spring,
WSR-88D PRECIPITATION ESTIMATION FOR HYDROLOGIC APPLICATIONS DENNIS A. MILLER.
Flash Flood Prediction Working Group Q2 Workshop June 28-30, 2005.
Agenda Introduction –What is FFMP? Foundation –Basic Components and Localization Common Problems –Often seen and easily fixed Troubleshooting Resources.
Introduction to Urban Hydrology
National Weather Service Hydrologic Forecasting Course Agenda 14 October – 7 November 2003.
An Assessment of the Use of AMBER in a Semi-Arid Desert Region Melissa A. Goering NOAA/NWS/Tucson, AZ Paul Jendrowski NOAA/NWS/Honolulu, HI.
Estimating Rainfall in Arizona - A Brief Overview of the WSR-88D Precipitation Processing Subsystem Jonathan J. Gourley National Severe Storms Laboratory.
BUILDING AND RUNNING THE HYDROLOGICAL MODEL
Digital model for estimation of flash floods using GIS
Multi-Sensor Precipitation Estimation
Elaine B. Darby GIS – Fall 2005
Hydrologic modeling of Waller Creek
Presentation transcript:

AMBER/FFMP Overview COMET Basin Customization August 2002 Robert S. Davis, Pittsburgh NWSWFO

AWIPS Flash Flood Monitoring and Prediction (FFMP) AWIPS build (Early 2002) the AMBER implementation of FFMP using DHR. Requires NSSL CD of ArcView defined watersheds and WSR-88D bin assignments. Provides graphic display of ABR and ABR–FFG for time periods of 30,60,90,120,180,360 minutes. Provides line graph of ABR,ABR Rate, and FFG for the same time periods. 1 level of streams supported FFMP small subset of AMBERGIS functionality.

FFMP Graphics County display of CWA-maximum ABR for any stream in county displayed. Left click on Fips code to get “stream display”. Stream display for a county- ABR for time period selected displayed for each basin. right click on stream ID to get “line graph”. Line graph of ABR + ABR Rate + FFG

Worthville, PA Flash Flood 05 June 2002 Jefferson County, PA

FFMP Text Data on AWIPS Where is your WSR-88D ID

FFMP file archiving ABR file is archived to hard disk on AWIPS for current GMT day and previous day only. + yyyymmdd.index for a GMT day Index file holds the time for each volume scan. Date file holds the ABR data for each stream (integer*2 data with a record length equal to 2 times the number of FFMP watersheds).

FFMP Basin Attributes /basinToCounty.dat /binToBasin.dat Radar bins are numbered consecutively from 0 to starting with radial 0.5 degrees. Bin 0 = 0.5 degrees at 0.5 km, bin 230 = 1.5 degrees at 0.5km, etc.

basinList.dat First line in file is number of basins (5609) Basin ID number in FFMP display is position in this file basin id =0 (2 nd line), 1 (3 rd line), 2 (4 th line), 3 (5 th line), etc. Pfafstetter ID Latitude/longitude of basin centroid Name of creek

binToBasin.dat First line is number of basins Second line is data for watershed id=0 1 st element (number of bins assigned) Bin number for each assigned bin follows, if 3 bins assigned to this stream, 3 bin numbers will be listed. Last element: area of bin summation (km 2 )

basinToCounty.dat Number of counties on first line Two letter state County name County Fips code Number of streams assigned to this county List of Basin Ids assigned to this county County assigned by MDL lat/lon of centroid

Stream Basin Definitions

National Basin Delineation 30Sep1999 – NWS agrees to fund the AMBER National Basin Delineation project by NSSL for all of the continental United States. ArcInfo used to define the watershed boundaries. USGS 1 arc second (30 m) DEM data supplied by EROS Data Center. Continental U.S. completed June 2002.

229.5 km Range ring NSSL Basins 18,488 Aggregated 12,784 Aggregate: Clip all basins beyond 230 km Eliminate all segments < 2 mi 2

FFMP Basins 5,608 NSSL CD FFMP

Purpose of the Basin Customization Course To describe the content of the NSSL dataset (ArcView shapefiles and data attributes). To provide tools that allow the local forecast office to modify, correct, or enhance the NSSL set of defined basins. To demonstrate why modifications or additions may enhance the application of FFMP to the flash flood warning process.

Choices: Customization Options No Customization (used delivered cd) Minor Customization (add stream names, make minor adjustments to basins to correct errors) Must still run localization. Major Customization (add new streams, divided existing streams) Paul’s procedure for hydrologic connectivity, allows use of Paul’s tools.

Choices: Display options at WFO Display FFMP graphics as delivered Run Paul Jendrowski’s AMBER for more stream layers, 7 AWIPS radar graphic products including ABR rate + 6 user selected time periods, AMBER browser, and line graph of past 6 hours. Use ArcView as display for geographic information.

Areal Mean Basin Estimated Rainfall ( AMBER) All watersheds in county warning area are defined to a Minimum Basin Area (MBA) of 2 mi 2 to show spatial rainfall distribution. The WSR-88D polar grid (1 o by 1 km) is mapped to the defined watersheds. Average Basin Rainfall (ABR) is computed for each watershed every volume scan. An hourly ABR rate is determined from the single volume scan (5-6 min.) of ABR.

AMBERGIS (2000 – 2002) Paul Jendrowski creation using ArcView. ABR data computed and archived (5 min). AWIPS ABR Rate display of radar umbrella. AWIPS ABR graphic display of radar umbrella for 6 user selected time periods. Line graph of ABR, ABR Rate, and FFG for each defined stream and rain gage. Nine layers of streams or rain gages supported. Alert for 3 user selected levels of ABR - FFG.

Graphical Radar Rainfall OHP – One hour rainfall STP – Storm total rainfall THP – Three hour rainfall

Storm Total Rainfall 19 May1999 Grid 1 o x 2km

AMBER/FFMP Digital Rainfall AMBER/FFMP computes 5 minute rainfall using WSR-88D precipitation algorithm with Digital Hybrid Scan Reflectivity (DHR) product as input.

Digital Hybrid Scan Reflectivity (DHR) Time interval (5-6 minutes) Grid size (1 degree x 1 km) Reflectivity to the nearest 0.5 dBZ

DHR Grid Area (km 2 ) vs. Radar Range (km)

DHR Digital Rainfall Estimate 2130 – 2135 UTC Rainfall (in) Grid size 1 o x 1km

DHR Digital Rainfall Estimate 2130 – 2135 UTC Rainfall (mm) Watershed Boundary…compute ABR

Average Basin Rainfall = – 2135 UTC ABR (in).29 Copy ABR back into DHR grid for FFMP or AMBERGIS graphics

Average Basin Rainfall = – 2135 UTC ABR (in) Divide watershed into segments??

Average Basin Rainfall =.29 in 2130 – 2135 UTC ABR (in) Large variation of ABR in short distances!!

Flash Flood Index (FF) FF = ABR - FFG Determining the Flash Flood Threat

Flash Flood Guidance (FFG) ABR in a specific time period (1, 3 hours) to initiate flooding on streams. Assumes stream at low flow level. Assumes no rainfall since data cutoff FFG is the amount of ABR needed to produce threshold runoff (climatic average runoff needed to start flooding of streams)

Flash Flood Guidance (FFG) FFG = TR + SM, where TR is the threshold runoff and SM is the amount of ABR needed to initiate runoff based on soil moisture content. Threshold runoff is constant for all watersheds 1.00” in three hours for most of eastern U.S (0.75” for western PA + WV). Ask your servicing RFC for your TR!!!

FF Index = ABR - FFG ABR and FFG in inches FF0 ABR = FFG FF1 ABR = FFG inches FF2 ABR = FFG inches FF3 ABR = FFG inches FF4 ABR = FFG inches FF5 ABR = FFG inches, etc

Noble County, OH Almost a flash flood. ABR-FFG = June UTC 1-Hour FFG = 1.70

FFMP Graphic Products vs. AMBERGIS Graphics

FFMP FFG

AMBER ABR-Rate AMBER 90-min ABR AMBER 120-min ABR

AMBER 60-min ABR

Change FFG Curve

Little Pine Creek Flash Flood 30 May 1986 ABR-FFG=5.0

Pine Creek Watershed 68 mi 2 ID Name Area 1000 L Pine Cr L Pine Cr Gourdhead Run Crouse Run Willow Run Montour Run NF Pine Cr Headwaters 13.9 Allegheny River Pine Creek Flash Flood Bucket Survey (inches) 30 May

Little Pine Creek 30 May 1986 Area: 6.2 mi 2 Little Pine Creek 30 May 1986 Area: 6.2 mi 2 Time (UTC)

Zion National Park Flash Flood 27 July 1998

3.30 1:30 1: :45 End of Trail Start of Trail Estimated hiking Time in hours. Deep Creek Kolob Creek Goose Creek Corral Hollow Orderville Canyon North Fork Virgin River The Narrows Hiking Trail Zion National Park, Utah Adapted from National Geographic Trails Illustrated “The Narrows” No safe high ground

Hiking in the “Narrows”

Washington County Kane County Iron County Orderville Canyon North Fork of the Virgin River Deep Creek The Narrows Kolob Creek EPA RF3 Data

Orderville Canyon Mouth into the Narrows

Deep Creek mi 2 NF Virgin River 70.3 mi 2 Orderville Canyon 41.5 mi 2 Kolob Creek 30.1 mi 2 Goose Cr 4.7 mi 2 Corral Hollow 2.2 mi 2 Imlay Canyon 3.8 mi 2 NF Virgin River above the Narrows 285 mi 2 The Narrows 4.1 mi 2 ABR (in) UTC 27 July km KICX WSR-88D 1-hour FFG 0.50

KICX WSR-88D 010km Deep Creek mi 2 NF Virgin River 70.3 mi 2 Orderville Canyon 41.5 mi 2 Kolob Creek 30.1 mi 2 NF Virgin River above the Narrows 285 mi 2 ABR (in) UTC 27 July hour FFG 0.50

1004 Goose Creek Corral Hollow Imlay Canyon North Fork of the Virgin River Orderville Canyon Deep Creek Kolob Creek North Fork of the Virgin River above the Narrows xx.x = miles above trail head The Narrows

Deep Creek (5) # July mi 2

Maximum Bin 176 o at 20 km 27July1998 Maximum rainfall on Storm Total Product 3.14 in.

Washington County Kane County mi mi mi mi mi 2 North Fork of the Virgin River above the Narrows 70.3 mi ABR (in) 27 July UTC “The Narrows” NF Virgin River (1-5) 3.14

NF Virgin River (2) # July mi 2

Washington County, UT Kane County, UT NF Virgin River Subdivisions Straight Canyon(1-3) NF Virgin River(2-4) 5006 Willow Canyon 5007 Hay Canyon 5008 Simon Gulch 5009 NF Virgin River(1) 5010 Rosy Canyon 5011 Stevens Canyon 5012 Ashdown Canyon ABR 27 July UTC 3.14

NF Virgin River(2) # July mi 2

NF Virgin River(3) # July mi 2

NF Virgin River(4) # July mi 2

Willow Canyon # July mi 2

Straight Canyon(2) # July mi 2

ABR Rates NF Virgin River 27July1998

AMBER Summary ABR provides basin specific rainfall to determine flash flood risk (ABR-FFG) ABR rate focuses forecaster attention on critical streams before flooding occurs. History (6-72 hours) of ABR helpful in adjusting FFG for multiple rainfall events. Basin specific ABR allows forecaster to mention “threat area” in warning text.

AMBER Data Sources ArcView and the spatial analyst extension. USGS Data (3 arc second DEM data) edcwww.cr.usgs.gov EPA Data (RF3 data files)

AMBER Case Studies buff.ppt 13Jul96 epgh99.ppt 18May99 pitcairn.ppt 01Jul97 zion.ppt 27Jul98 ohio98.ppt 26Jun98 redbank.ppt 19Jul96 dallas95.ppt 05May95 ftc97.ppt 28Jul97 kc1998.ppt 05Oct98 Buffalo Creek, CO Pittsburgh, PA Cedar City, UT Eastern Ohio Brookville, PA* Dallas, TX* Fort Collins, CO* Kansas City, MO* * Tropical Z/R Cases