Kick-Off-Treffen PQP 23./24. Oktober Bonn QUEST Partnership  Susanne Crewell, Thorsten Reinhardt, University of Cologne (UC)  Jürgen Fischer, Anja Hünerbein,

Slides:



Advertisements
Similar presentations
Quantitative evaluation of regional precipitation forecasts using multi-dimensional remote sensing observations (QUEST) Nicole van Lipzig a, Susanne Crewell.
Advertisements

Kick-Off-Treffen PQP 23./24. Oktober Bonn GOP Partnership Karl Bumke (IFM-Geomar) Disdrometer observations (WP 3) Susanne Crewell (IGM)Overall GOP organisation.
Institut für Physik der Atmosphäre Life Cycle of Deep Convection during the COPS Field Campaign (LIFCOC) Martin Hagen, Hartmut Höller, George Craig Institut.
Estimation of clouds in atmospheric models Tomislava Vukicevic CIRA/CSU and PAOS/CU.
Ewan OConnor, Robin Hogan, Anthony Illingworth Drizzle comparisons.
R. Forbes, 17 Nov 09 ECMWF Clouds and Radiation University of Reading ECMWF Cloud and Radiation Parametrization: Recent Activities Richard Forbes, Maike.
Anthony Illingworth, + Robin Hogan, Ewan OConnor, U of Reading, UK and the CloudNET team (F, D, NL, S, Su). Reading: 19 Feb 08 – Meeting with Met office.
Integrated Profiling at the AMF
Marc Schröder et al., FUB BBC2 Workshop, De Bilt, 10.´04 Problems related to absorption dependent retrievals and their validation Marc Schröder 1, Rene.
Development of Data Assimilation Systems for Short-Term Numerical Weather Prediction at JMA Tadashi Fujita (NPD JMA) Y. Honda, Y. Ikuta, J. Fukuda, Y.
Introduction to data assimilation in meteorology Pierre Brousseau, Ludovic Auger ATMO 08,Alghero, september 2008.
1 October 26, th COPS Workshop, Cambridge, UK COPS (Convective and Orographically-induced Precipitation Study) Goal: Advance the quality of forecasts.
COSMO Workpackage No First Results on Verification of LMK Test Runs Basing on SYNOP Data Lenz, Claus-Jürgen; Damrath, Ulrich
WMO International Cloud Modeling Workshop, July 2004 A two-moment microphysical scheme for mesoscale and microscale cloud resolving models Axel Seifert.
Lidar-Based Microphysical Retrievals During M-PACE Gijs de Boer Edwin Eloranta The University of Wisconsin - Madison ARM CPMWG Meeting, October 31, 2006.
TRMM Tropical Rainfall Measurement (Mission). Why TRMM? n Tropical Rainfall Measuring Mission (TRMM) is a joint US-Japan study initiated in 1997 to study.
Daily runs and real time assimilation during the COPS campaign with AROME Pierre Brousseau, Y. Seity, G. Hello, S. Malardel, C. Fisher, L. Berre, T. Montemerle,
Institut für Physik der Atmosphäre Predictability of precipitation determined by convection-permitting ensemble modeling Christian Keil and George C.Craig.
Atmospheric structure from lidar and radar Jens Bösenberg 1.Motivation 2.Layer structure 3.Water vapour profiling 4.Turbulence structure 5.Cloud profiling.
Rapid Update Cycle Model William Sachman and Steven Earle ESC452 - Spring 2006.
Spatial and temporal variability of drop size distribution from vertically pointing micro rain radar (MRR) Clemens Simmer 1 and Malte Diederich 1 Presented.
The use of radar in evaluating precipitation in LMK and ARPS: two precipitation cases over Belgium 6 March 2007 International PhD-studens and Post-docs.
Quantitative evaluation of regional precipitation forecasts for Belgium using multi-dimensional remote sensing observations (QUEST-B) Nicole van Lipzig.
Institut für Physik der Atmosphäre Status of working group Precipitation Processes and Live cycle Martin Hagen DLR Oberpfaffenhofen.
Institut für Physik der Atmosphäre POLDIRAD Polarization Diversity Doppler Radar Martin Hagen DLR Oberpfaffenhofen.
Quantitative evaluation of regional precipitation forecasts for Belgium using multi-dimensional remote sensing observations (QUEST-B) Nicole van Lipzig.
Ensemble Post-Processing and it’s Potential Benefits for the Operational Forecaster Michael Erickson and Brian A. Colle School of Marine and Atmospheric.
Assimilation of (satellite) cloud-information at the convective scale in an Ensemble Kalman Filter Annika Schomburg 1, Christoph Schraff 1, Africa Perianez.
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
Remote-sensing of the environment (RSE) ATMOS Analysis of the Composition of Clouds with Extended Polarization Techniques L. Pfitzenmaier, H. Russchenbergs.
WMO Cloud Modelling Workshop, Hamburg, 12. Juli 2004 The BALTEX BRIDGE Campaign (BBC) cases Susanne Crewell, Nicole van Lipzig, Wenchieh Yen Meteorological.
SMHI in the Arctic Lars Axell Oceanographic Research Unit Swedish Meteorological and Hydrological Institute.
Introducing the Lokal-Modell LME at the German Weather Service Jan-Peter Schulz Deutscher Wetterdienst 27 th EWGLAM and 12 th SRNWP Meeting 2005.
COSMO General Meeting, Offenbach, 7 – 11 Sept Dependance of bias on initial time of forecasts 1 WG1 Overview
Slide 1 Impact of GPS-Based Water Vapor Fields on Mesoscale Model Forecasts (5th Symposium on Integrated Observing Systems, Albuquerque, NM) Jonathan L.
The Role of Polarimetric Radar for Validating Cloud Models Robert Cifelli 1, Timothy Lang 1, Stephen Nesbitt 1, S.A. Rutledge 1 S. Lang 2, and W.K. Tao.
Non-hydrostatic Numerical Model Study on Tropical Mesoscale System During SCOUT DARWIN Campaign Wuhu Feng 1 and M.P. Chipperfield 1 IAS, School of Earth.
Estimation of Cloud and Precipitation From Warm Clouds in Support of the ABI: A Pre-launch Study with A-Train Zhanqing Li, R. Chen, R. Kuligowski, R. Ferraro,
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Southern Ocean cloud biases in ACCESS.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss WG 3: Overview status report COSMO General Meeting, 19.
Three real case simulations by Meso-NH validated against satellite observations J.-P. Chaboureau and J.-P. Pinty Laboratoire d’Aérologie, Toulouse 1.Elbe.
Aktionsprogramm Thorsten Reinhardt, DWD Sensitivity Tests Regarding Assumed Graupel Particle Properties Motivation: Gilmore et al (MWR 2004) found.
Investigations of Artifacts in the ISCCP Datasets William B. Rossow July 2006.
DRAFT – Page 1 – January 14, 2016 Development of a Convective Scale Ensemble Kalman Filter at Environment Canada Luc Fillion 1, Kao-Shen Chung 1, Monique.
Meteorologisches Institut der Universitat Munchen A shallow convection case from BBC: Results from the WMO international cloud modelling workshop Nicole.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Poster Presentation Working Group 3: Physical Aspects.
Joint SRNWP/COST-717 WG-3 session, Lisbon Stefan Klink Data Assimilation Section Early results with rainfall assimilation.
Basis of GV for Japan’s Hydro-Meteorological Process Modelling Research GPM Workshop Sep. 27 to 30, Taipei, Taiwan Toshio Koike, Tobias Graf, Mirza Cyrus.
Vincent N. Sakwa RSMC, Nairobi
Philippe Steiner, MeteoSwiss COSMO General Meeting September 22th, 2005 Plans of MeteoSwiss for next year.
Remote sensing and modeling of cloud contents and precipitation efficiency Chung-Hsiung Sui Institute of Hydrological Sciences National Central University.
Active and passive microwave remote sensing of precipitation at high latitudes R. Bennartz - M. Kulie - C. O’Dell (1) S. Pinori – A. Mugnai (2) (1) University.
UCLA Vector Radiative Transfer Models for Application to Satellite Data Assimilation K. N. Liou, S. C. Ou, Y. Takano and Q. Yue Department of Atmospheric.
Land-Surface evolution forced by predicted precipitation corrected by high-frequency radar/satellite assimilation – the RUC Coupled Data Assimilation System.
COSMO model simulations for COPS IOP 8b, 15 July 2007 Jörg Trentmann, Björn Brötz, Heini Wernli Institute for Atmospheric Physics, Johannes Gutenberg-University.
Assimilating Cloudy Infrared Brightness Temperatures in High-Resolution Numerical Models Using Ensemble Data Assimilation Jason A. Otkin and Rebecca Cintineo.
Mesoscale Assimilation of Rain-Affected Observations Clark Amerault National Research Council Postdoctoral Associate - Naval Research Laboratory, Monterey,
Joint MAP D-PHASE Scientific Meeting - COST 731 mid-term seminar, May 2008, Bologna. ErgebnissErgebniss : Long-Term Evaluation of COSMO-DE and COSMO-EU.
Introducing the Lokal-Modell LME at the German Weather Service
Recent GNSS activities in Germany for COST and E-GVAP
Structure of the general part
Results for the COPS Region
Tadashi Fujita (NPD JMA)
Simulation of the Arctic Mixed-Phase Clouds
Three-category ice scheme
Daniel Leuenberger1, Christian Keil2 and George Craig2
Short Term forecasts along the GCSS Pacific Cross-section: Evaluating new Parameterizations in the Community Atmospheric Model Cécile Hannay, Dave Williamson,
NWP Strategy of DWD after 2006 GF XY DWD Feb-19.
Preliminary validation results of the prognostic 3d-TKE-scheme
Presentation transcript:

Kick-Off-Treffen PQP 23./24. Oktober Bonn QUEST Partnership  Susanne Crewell, Thorsten Reinhardt, University of Cologne (UC)  Jürgen Fischer, Anja Hünerbein, FU Berlin (FUB)  George Craig, Martin Hagen, Monika Pfeifer, (DLR)  Michael Baldauf, Deutscher Wetterdienst (DWD)  Nicole van Lipzig, Katholieke Universiteit Leuven (KUL), Belgium Quantitative evaluation of regional precipitation forecasts using multi-dimensional remote sensing observations Contributes to PQP Goals  Identification of physical and chemical processes responsible for the deficiencies in quantitative precipitation forecast  Determination and use of the potentials of existing and new data and process descriptions to improve quantitative precipitation forecast

Kick-Off-Treffen PQP 23./24. Oktober Bonn LE satellite MSG ~ 5km; 15min  Cloud Mask  Cloud top pressure MODIS ~ 1km; 1day  Cloud Mask  Optical thickness IPT / Micro- wave 1D vertical; Lindenberg (and Cabauw)  temperature profile  humidity profile  LWC GPS 147 stations; Germany; 30min  IWV Ceilometer 17 stations; Germany; 1min; ranges up to 4km  Cloud base height  Cloud cover (<4km) Radar DX radar composite; 1km; 5min  Rain rate Polarimetric radar (DLR) Combining different remote sensing techniques

Kick-Off-Treffen PQP 23./24. Oktober Bonn QUEST: Strategy Observations - multi-frequency radiances - polarimetric radar quantities - ground based and space borne observations Forward OperatorRetrieval Weather Forecasts - three-dimensional description of the forecasted atmospheric state - focus on Lokal-Modell Kürzestfrist (LMK) - SynPolRad (polari. radar) - SynSat (MSG, MODIS) - SynSatMic (AMSU, SSM/I) - water vapour - cloud properties - precipitation Schröder et al. [2006]

Kick-Off-Treffen PQP 23./24. Oktober Bonn QUEST: Approach Case Studies (ongoing) Model Sensitivity Runs Tool development  SynPolRad  SynSat (-Mic)  MSG µ-phys. retrievals  verification measures .. Hypothesis formulation "What are the crucial variables/processes to observe and to improve?" Model Improvement (new)  cloud microphysics  land surface  turbulence comparison tools test of hypotheses Identification of systematic model deficits Long Term Evaluation Lokal-Modell Kürzestfrist  test suites  GOP duration 2007  benefits of high resolution modelling Conditional verification  regionalization  diurnal cycle  weather situation dep. Cross correlation of different variables "How important is physical consistency?" case study selection for process studies

Kick-Off-Treffen PQP 23./24. Oktober Bonn Van Lipzig et al.: “Model predicted low-level cloud parameters. Part I: Comparison with observations from the BALTEX Bridge Campaigns”, Atmospheric Research, accepted Vertical structure  Shallow convection scheme gives no significant benefit.  LM underestimates the life-time of clouds.  LM has deficiencies to represent small- scale cloud structures. PQP Phase 1: Case study 23 Sep. 2001

Kick-Off-Treffen PQP 23./24. Oktober Bonn PQP Phase 1: Case study 23 Sep Schröder et al.: “Model predicted low-level cloud parameters. Part II: Comparison with satellite remote sensing observations during the BALTEX Bridge Campaigns”, Atmospheric Research, acc. Horizontal structure: MODIS LM cloud cover τ  Modeled and observed cloud structure are different.  LM underestimates clouds with moderate LWC / optical depth.  Shallow convection scheme gives no significant benefit.

Kick-Off-Treffen PQP 23./24. Oktober Bonn Reflectivity differential reflectivity ZDR Linear depola- risation ratio LDR Sensitive to rain Sensitive to ice particles Polarimetric radar quantities  Forward operator SynPolRad links LM predictions and observations.  Polarimetric data provides information about hydrometeor types.  Inclusion of graupel in LMK improves representation of convective cells. No graupelgraupel  add more observations for better constraints  test more microphysical schemes Pfeifer, M., Craig, G., Hagen, M. and Keil, C.: “A polarimetric forward operator”, Proceeding of ERAD 2004, PQP Phase 1: Case study 12 Aug. 2004

Kick-Off-Treffen PQP 23./24. Oktober Bonn Lokal-Modell Kürzestfrist (LMK) Testsuite 2.2b: July 2004  Prognostic treatment of cloud water, cloud ice, rain and snow  2.8km horizontal resolution, 50 vertical levels LMK domain Pre-operational phase may 2006 – spring 2007 Operational expected spring 2007 Lagged average forecast ensemble Day 1 00UTC Day 2 00UTC Day 3 00UTC Day 1 12UTC Day 2 12UTC

Kick-Off-Treffen PQP 23./24. Oktober Bonn Conditional Verification: LTE  complete test suites analysis  separate weather regimes  cross correlate variables  prepare GOP exploitation Cloud cover (%) LMK00 / LMK12 BIAS (%)STD (%)Correlation LMK total8 / 59 / / 0.80 Sea9 / 817 / / 0.70 Alps6 / 214 / / 0.81 Flat land9 / 717 / / 0.70 Low mountain7 / 515 / / 0.67 Poldirad domain5 / 217 / / 0.75 COPS domain4 / 022 / / 0.61 MSG Comparison: July 2004

Kick-Off-Treffen PQP 23./24. Oktober Bonn Daily cycle of accumulated precipitation over the month compared to radar % Accumulated precipitation Relative bias in accumulated precipitation over the month compared to radar

Kick-Off-Treffen PQP 23./24. Oktober Bonn Summary of long term evaluation of LMK LE  Boundary layer too thin and too wet  IWV predicted very well  IWV bias of kg/m2 for run started at 12UTC  Clouds too thick  Total cloud cover agrees well with MSG  Precipitation underestimated by 20%  Observed timing maximum not reproduced Case studies to look into more detail in the problems

Kick-Off-Treffen PQP 23./24. Oktober Bonn PQP Collaborations Improvement of Model Physics  Beheng and Blahak, Karlsruhe Test of the newly developed cloud microphysics parametrization  Bott, Küll and Gassmann, Bonn Evaluation of the newly developed convection scheme, case study selection Verification  Cubasch, Nevir and Reimer, Berlin (STAMPF) Verification measures, precipitation analysis, satellite data, connection to clouds and vertical velocity  Wernli, Hagen and Frei, Mainz (VERIPREG) Verification measures, aggregated radar products, cross correlation of variables Data assimilation  Simmer et al., Bonn (DAQUA) Identification of test cases, satellite data, verification of assimilation runs COPS & GOP Preparation