Using Probalistic Quantitative Precipitation Forecasts PQPFs within a hydro-meteorological chain within a hydro-meteorological chain R. Marty, A. Djerboua,

Slides:



Advertisements
Similar presentations
Streamflow assimilation for improving ensemble streamflow forecasts G. Thirel (1), E. Martin (1), J.-F. Mahfouf (1), S. Massart (2), S. Ricci (2), F. Regimbeau.
Advertisements

Medium-range Ensemble Streamflow forecast over France F. Rousset-Regimbeau (1), J. Noilhan (2), G. Thirel (2), E. Martin (2) and F. Habets (3) 1 : Direction.
On the importance of meteorological downscaling for short, medium and long-range hydrological ensemble prediction over France G. Thirel (1), F. Regimbeau.
Description and validation of a streamflow assimilation system for a distributed hydrometeorological model over France. Impacts on the ensemble streamflow.
RSMC La Réunion activities regarding SWFDP Southern Africa Matthieu Plu (Météo-France, La Réunion), Philippe Arbogast (Météo-France, Toulouse), Nicole.
SH - SYSTEM of HYDROLOGY Grzegorz SLOTA Head of the Section System of Hydrology (SH).
Nowcasting and Short Range NWP at the Australian Bureau of Meteorology
Introduction to data assimilation in meteorology Pierre Brousseau, Ludovic Auger ATMO 08,Alghero, september 2008.
Hydrological information systems Svein Taksdal Head of section, Section for Hydroinformatics Hydrology department Norwegian Water Resources and Energy.
QPF verification of the 4 model versions at 7 km res. (COSMO-I7, COSMO-7, COSMO-EU, COSMO-ME) with the 2 model versions at 2.8 km res. (COSMO- I2, COSMO-IT)
Report of the Q2 Short Range QPF Discussion Group Jon Ahlquist Curtis Marshall John McGinley - lead Dan Petersen D. J. Seo Jean Vieux.
4 th International Symposium on Flood Defence Generation of Severe Flood Scenarios by Stochastic Rainfall in Combination with a Rainfall Runoff Model U.
CHARACTERISTICS OF RUNOFF
MAP D-PHASE Forecast Demonstration Project Instrument of WWRP Last phase of MAP Mathias Rotach, MeteoSwiss.
Towards an Hydrological Qualification of the Simulated Rainfall in Mountainous Areas Eddy Yates, Sandrine Anquetin, Jean-Dominique Creutin Laboratoire.
2012: Hurricane Sandy 125 dead, 60+ billion dollars damage.
Data assimilation of trace gases in a regional chemical transport model: the impact on model forecasts E. Emili 1, O. Pannekoucke 1,2, E. Jaumouillé 2,
PROVIDING DISTRIBUTED FORECASTS OF PRECIPITATION USING A STATISTICAL NOWCAST SCHEME Neil I. Fox and Chris K. Wikle University of Missouri- Columbia.
Precipitation statistics Cumulative probability of events Exceedance probability Return period Depth-Duration-Frequency Analysis.
Univ of AZ WRF Model Verification. Method NCEP Stage IV data used for precipitation verification – Stage IV is composite of rain fall observations and.
The Consideration of Noise in the Direct NWP Model Output Susanne Theis Andreas Hense Ulrich Damrath Volker Renner.
Ensemble Post-Processing and it’s Potential Benefits for the Operational Forecaster Michael Erickson and Brian A. Colle School of Marine and Atmospheric.
Colorado Basin River Forecast Center Water Supply Forecasting Method Michelle Stokes Hydrologist in Charge Colorado Basin River Forecast Center April 28,
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Synthetic future weather time-series at the local scale.
Operationnal use of high resolution model AROME image source: Sander Tijm, KNMI.
Water Supply Forecast using the Ensemble Streamflow Prediction Model Kevin Berghoff, Senior Hydrologist Northwest River Forecast Center Portland, OR.
Hydrologic Statistics
Inclusion of potential vorticity uncertainties into a hydrometeorological forecasting chain: Application to a flash-flood event over Catalonia, Spain A.
Downscaling in time. Aim is to make a probabilistic description of weather for next season –How often is it likely to rain, when is the rainy season likely.
Numerical simulations of the severe rainfall in Pula, Croatia, on 25 th September 2010 Antonio Stanešić, Stjepan Ivatek-Šahdan, Martina Tudor and Dunja.
1 Flood Hazard Analysis Session 1 Dr. Heiko Apel Risk Analysis Flood Hazard Assessment.
Application of a rule-based system for flash flood forecasting taking into account climate change scenarios in the Llobregat basin EGU 2012, Vienna Session.
STEPS: An empirical treatment of forecast uncertainty Alan Seed BMRC Weather Forecasting Group.
Evaluation of climate change impact on soil and snow processes in small watersheds of European part of Russia using various scenarios of climate Lebedeva.
WORKSHOP ON SHORT-RANGE ENSEMBLE PREDICTION USING LIMITED-AREA MODELS Instituto National de Meteorologia, Madrid, 3-4 October 2002 Limited-Area Ensemble.
June 16th, 2009 Christian Pagé, CERFACS Laurent Terray, CERFACS - URA 1875 Julien Boé, U California Christophe Cassou, CERFACS - URA 1875 Weather typing.
Hydrological extremes and their meteorological causes András Bárdossy IWS University of Stuttgart.
SPATIO-TEMPORAL STATIONARITY OF THE MEAN RAINFALL Armand NZEUKOU University of Dschang Cameroon & Henri SAUVAGEOT University of Toulouse III France.
Celeste Saulo and Juan Ruiz CIMA (CONICET/UBA) – DCAO (FCEN –UBA)
Flash Floods in a changing context: Importance of the impacts induced by a changing environment.
Hydrometeorological Prediction Center HPC Experimental PQPF: Method, Products, and Preliminary Verification 1 David Novak HPC Science and Operations Officer.
Flash flood forecasting in Slovakia Michal Hazlinger Slovak Hydrometeorological Institute Ljubljana
July 5-9, 2009, Univ. of Bologna, Italy HARP - A Software Tool for Fast Assessment of Radiation Accident Consequences and their Variability Petr Pecha.
Typhoon Forecasting and QPF Technique Development in CWB Kuo-Chen Lu Central Weather Bureau.
Hydrological forecasting: application, uncertainty, estimation, data assimilation and decision making EGU – Wien, 7th april 2011 The Po flood management.
The uncertainty in the prediction of flash floods in the Northern Mediterranean environment; single site approach and multi-catchment system approach CIMA.
Barcelona Toward an error model for radar quantitative precipitation estimation in the Cévennes- Vivarais region, France Pierre-Emmanuel Kirstetter, Guy.
MRC-MDBC STRATEGIC LIAISON PROGRAM BASIN DEVELOPMENT PLANNING TRAINING MODULE 3 SCENARIO-BASED PLANNING for the MEKONG BASIN Napakuang, Lao PDR 8-11 December.
DOWNSCALING GLOBAL MEDIUM RANGE METEOROLOGICAL PREDICTIONS FOR FLOOD PREDICTION Nathalie Voisin, Andy W. Wood, Dennis P. Lettenmaier University of Washington,
Pearl River Coordination Meeting October 7, 2009 Dave Reed Hydrologist in Charge Lower Mississippi River Forecast Center.
WATER RESOURCES DEPARTMENT
Numerical simulations of the severe rainfall in Pula, Croatia, on 25 th September 2010 Antonio Stanešić, Stjepan Ivatek-Šahdan, Martina Tudor and Dunja.
Performance assessment of a Bayesian Forecasting System (BFS) for realtime flood forecasting Biondi D. , De Luca D.L. Laboratory of Cartography and Hydrogeological.
K. Chancibault, V. Ducrocq, F. Habets CNRM/GAME, Météo-France
Xuexing Qiu and Fuqing Dec. 2014
AMPHORE - Interreg III B Medocc
Mediterranean Meeting on ″Monitoring, modelling and early warning of extreme events triggered by heavy rainfalls″. MED-FRIEND project. University of Calabria,
Hydrologic Considerations in Global Precipitation Mission Planning
Daniela Rezacova, Zbynek Sokol IAP ASCR, Prague, Czech Republic
Meteorological and Hydrological Service of Croatia
Methodology to integrate dynamical and statistical weather forecasts
Al Cope National Weather Service Forecast Office Mount Holly, NJ  
Nathalie Voisin, Andy W. Wood and Dennis P. Lettenmaier
Overview of Models & Modeling Concepts
Thomas Gastaldo, Virginia Poli, Chiara Marsigli
Hydrological Forecasting Service
Evaluating Satellite Rainfall Products for Hydrological Applications
Verifying Ensemble Forecasts
SRNWP-PEPS COSMO General Meeting September 2005
Hydrology and Precipitation (a review and application)
Presentation transcript:

Using Probalistic Quantitative Precipitation Forecasts PQPFs within a hydro-meteorological chain within a hydro-meteorological chain R. Marty, A. Djerboua, Ch. Obled & I. Zin LTHE - INPG, Grenoble - France.

I. General Organization of the chain  The different modules required  Meteorological forecasts and processing II. Generation / disagregations of rainfall scenarios  Principle and architecture of the generator  Conditioning by the past (as observed)  Conditioning by the future (as forecast) Plan : A Hydro-meteorological Chain IV. Conclusions & Perspectives Real Time Operation III.  Case study (Ardèche 2000)  Updating/refreshing of the forecasts

Chain: Modules

Forecast Suppliers Deterministic : Deterministic : 1 model / 1 trace Ensemble / Probabilistic : Ensemble / Probabilistic : 1 model / multiple traces Lead time Nowcasting Nowcasting 0h  3h (Radar) Short term forecasting Short term forecasting 6h -18h / 18h – 30 or 6h h But…! Requires Adaptation (for basin rainfall, etc…) (for basin rainfall, etc…) Chain: Meteo. Forecasts

Selecting a Forecast e.g. ECMWF or ARPEGE… + Adaptation + Adaptation e.g. ANALOG  PQPF Probabilistic precip. Forecast totalized on time-steps ∆ Mt FutureScenarios (hyeto.) Future Scenarios (hyeto.) conditioned by the PQPF ~ rainfall ‘‘Traces’’ at  Ht ~ rainfall ‘‘Traces’’ at  Ht eventually spatio-temporal… Hydrological Models Disagregation Meteo If : Meteo model time-step (24h) ∆ Ht (1h) ∆ Mt (24h) >> ∆ Ht (1h) Hydro Hydro model time-step Disagregation at ∆ Ht Then Disagregation at ∆ Ht via Rainfall Generator e.g.: via Rainfall Generator Temporal / spatio-temporal ? Chain: Processing

Rainfall generation / disagregation: Purposes : to be able to: generate « plausible » intense rainfall events propose an extension for a current event respect a rainfall forecast … + If forecast probabilistic (PQPF): + If forecast probabilistic (PQPF): distribution respect a distribution of future rainfall… Generator: Principles

Requires at least : ~ 20 events  statistical laws of these parameters Description and characterization of a rain event P(mm) t(h) Generator: Principles

Generator: Cond. Past

Number of wanted scenarios e.g. 500~1000 X Probability density PQPF of 24h totals issued at 6h Taking into account a Probabilistic Quantitative Precipitation Forecast Number of scenarios to retain for each class Generator: Cond. future

Calculation of the total on fixed 24h (06-06h UT) 42mm on 24h Scenario conditioned by the past Generator: Cond. future

42mm en 24h Number of scenarios to collect for each class Selection or Rejection of the scenario Retain this generated scenario for the class [40-45]mm except if there are already 120 Generator: Cond. future

Ardèche at Vogüé 635 km² Event of 12 th Nov.2000 Real Time:Ardèche 2000 Real Time: Ardèche 2000

Sunday Nov. 12 th at 6h UTC (adapted PQPF’s) distributions of precipitation forecast D for Nov. 12 th Observed rainfall over 24h Analog distribution 99.6 mm future real rainfall observed rainfall observed discharge simulated discharge quantile Real Time:Ardèche 2000 Real Time: Ardèche 2000

Eg.: ingredient available : a meteo forecast, every 24h (resp. 12h ou 6h…) day DF1(x) i.e. the precipitation distribution for day D  F1(x) day D+1F2(x) + the precipitation distribution for day D+1  F2(x) 24h IF required lead-time is « at least 12 h ahead » and if the updating cycle is 24h, then rainfall scenarios are conditioned as follow :  by PQPF precipitation distribution day D F1(x) of day D i.e. F1(x)  and by the sum of the distributions day Dday D+1F1 + F2(x) for day D & day D+1 i.e. F1 + F2(x) For 13 ~ 24h : For time-steps 13 ~ 24h : For 1 ~ 12h : For time-steps 1 ~ 12h : Real Time Real Time: Updating

distributions of precipitation forecast D for Nov. 12 th Analog distribution Day D D+1 for Nov. 13 th Analog distribution Day D+1 D  D mm Observed rainfall over 24h Analog distribution D  D+1 Observed rainfall over 48h Analog distribution : sum Days D & D mm D  D+1 Observed rainfall over 48h Analog distribution Sunday Nov. 12 th at 18h UTC 31.5 mm68.1 mm future real rainfall observed rainfall observed discharge simulated discharge quantile Real Time Real Time: Updating

Monday Nov. 13th at 6h TU New forecast (adapted PQPF’s) Refreshing : Distribution of precipitation forecast for the Nov. 13 th Observed rainfall over 24h Analog distribution 58.3 mm future real rainfall observed rainfall observed discharge simulated discharge quantile Real Time:Refreshing Real Time: Refreshing

Conclusions and Perspectives assimilationofPQPF from the analog method assimilation of Probabilistic Quant. Precip. Forecasts PQPF from the analog method to produce PQDF to produce Probabilistic Quant. Discharge Forecasts PQDF with a more appropriate time-step via a rainfall generator take into account operational constraints which take into account operational constraints hourly updating and daily refreshing  meteorological uncertainties and propagation also with ensemble meteorological forecasts  hydrological model uncertainties multi-model technique  rainfall generator regionalisation

Thanks for your attention !

For each episode : we consider at first NA NA : Storms number Principle and architecture of the generator Then for each storm :  DA  DA : Storm duration ITEA  ITEA : Duration of the dry period between storms HPA  HPA : Rainfall total of the storm HPMX  HPMX : Maximum of hourly rainfall HEMA  HEMA : Position of the maximum of hourly rainfall

Draw of the storms number : NA t Principle and architecture of the generator

t Draws of storms and Inter-storm durations : DA - ITEA Principle and architecture of the generator

Draws of rainfall totals: HPA = f(DA) t Principle and architecture of the generator

Draws of the maximum positions: HEMA Draws of the maximum hourly intensities : HPMX RPON = RPA/DA n  RPA = HPMX/HPA = G(DA)

Repartition of the storm volume HPA around HPMX Principle and architecture of the generator