Incorporation of TAMDAR into Real-time Local Modeling Tom Hultquist Science & Operations Officer NOAA/National Weather Service Marquette, MI.

Slides:



Advertisements
Similar presentations
A Cloud Resolving Model with an Adaptive Vertical Grid Roger Marchand and Thomas Ackerman - University of Washington, Joint Institute for the Study of.
Advertisements

5/18/2015 Prediction of the 10 July 2004 Beijing Flood with a High- Resolution NWP model Ying-Hwa Kuo 1 and Yingchun Wang 2 1. National Center for Atmospheric.
Rapid Refresh and RTMA. RUC: AKA-Rapid Refresh A major issue is how to assimilate and use the rapidly increasing array of off-time or continuous observations.
Transitioning unique NASA data and research technologies to the NWS 1 AIRS Products for the National Weather Service Brad Zavodsky SPoRT Science Advisory.
Recent performance statistics for AMPS real-time forecasts Kevin W. Manning – National Center for Atmospheric Research NCAR Earth System Laboratory Mesoscale.
Rapid Update Cycle Model William Sachman and Steven Earle ESC452 - Spring 2006.
Huang et al: MTG-IRS OSSEMMT, June MTG-IRS OSSE on regional scales Xiang-Yu Huang, Hongli Wang, Yongsheng Chen and Xin Zhang National Center.
Roll or Arcus Cloud Supercell Thunderstorms.
Transitioning unique NASA data and research technologies to the NWS 1 Evaluation of WRF Using High-Resolution Soil Initial Conditions from the NASA Land.
SNOWIN’ TO BEAT THE BAND Using Satellite and Local Analysis and Prediction System Output to Diagnose the Rapid Development of a Mesoscale Snow Band Eleanor.
Development of an eastern Great Lakes sub-regional WRF ensemble for lake effect snow prediction.
FORECASTING EASTERN US WINTER STORMS Are We Getting Better and Why? Jeff S. Waldstreicher NOAA/NWS Eastern Region Scientific Services Division – Bohemia,
Atmospheric Modeling at RENCI Brian J. Etherton. Atmospheric Modeling at RENCI Focus of RENCI for C- STAR project is to provide modeling support/development.
Consortium Meeting June 3, Thanks Mike! Hit Rates.
Roll or Arcus Cloud Squall Lines.
Impact of the 4D-Var Assimilation of Airborne Doppler Radar Data on Numerical Simulations of the Genesis of Typhoon Nuri (2008) Zhan Li and Zhaoxia Pu.
OAQPS Air Quality Modeling Group Fine-scale Meteorological Simulation of Cold Pools in Salt Lake City Chris Misenis, Kirk Baker, Pat Dolwick October 29,
“1995 Sunrise Fire – Long Island” Using an Ensemble Kalman Filter to Explore Model Performance on Northeast U.S. Fire Weather Days Michael Erickson and.
Climatology and Predictability of Cool-Season High Wind Events in the New York City Metropolitan and Surrounding Area Michael Layer School of Marine and.
Warn on Forecast Briefing September 2014 Warn on Forecast Brief for NCEP planning NSSL and GSD September 2014.
The Sensitivity of a Real-Time Four- Dimensional Data Assimilation Procedure to Weather Research and Forecast Model Simulations: A Case Study Hsiao-ming.
The National Environmental Agency of Georgia L. Megrelidze, N. Kutaladze, Kh. Kokosadze NWP Local Area Models’ Failure in Simulation of Eastern Invasion.
November 1, 2013 Bart Brashers, ENVIRON Jared Heath Bowden, UNC 3SAQS WRF Modeling Recommendations.
Using Fractional Lake Ice and Variable Ice Thickness in the WRF- ARW to improve Great Lakes Forecasting Michael Dutter and Todd Kluber NOAA/National Weather.
In this study, HWRF model simulations for two events were evaluated by analyzing the mean sea level pressure, precipitation, wind fields and hydrometeors.
A. FY12-13 GIMPAP Project Proposal Title Page version 27 October 2011 Title: Probabilistic Nearcasting of Severe Convection Status: New Duration: 2 years.
winter RADIATION FOGS at CIBA (Spain): Observations compared to WRF simulations using different PBL parameterizations Carlos Román-Cascón
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.
GLFE Status Meeting April 11-12, Presentation topics Deployment status Data quality control Data distribution NCEP meeting AirDat display work Icing.
Higher Resolution Operational Models. Operational Mesoscale Model History Early: LFM, NGM (history) Eta (mainly history) MM5: Still used by some, but.
WINDSOR TORNADO STUDY - STMAS (updated 9/16/2009 by Huiling Yuan and Yuanfu Xie)
AMB Verification and Quality Control monitoring Efforts involving RAOB, Profiler, Mesonets, Aircraft Bill Moninger, Xue Wei, Susan Sahm, Brian Jamison.
Earth-Sun System Division National Aeronautics and Space Administration SPoRT SAC Nov 21-22, 2005 Regional Modeling using MODIS SST composites Prepared.
Experiences with 0-36 h Explicit Convective Forecasting with the WRF-ARW Model Morris Weisman (Wei Wang, Chris Davis) NCAR/MMM WSN05 September 8, 2005.
P1.85 DEVELOPMENT OF SIMULATED GOES PRODUCTS FOR GFS AND NAM Hui-Ya Chuang and Brad Ferrier Environmental Modeling Center, NCEP, Washington DC Introduction.
Seasonal Modeling (NOAA) Jian-Wen Bao Sara Michelson Jim Wilczak Curtis Fleming Emily Piencziak.
Comparing GEM 15 km, GEM-LAM 2.5 km and RUC 13 km Model Simulations of Mesoscale Features over Southern Ontario 2010 Great Lakes Op Met Workshop Toronto,
Are Numerical Weather Prediction Models Getting Better? Cliff Mass, David Ovens, and Jeff Baars University of Washington.
Impact of FORMOSAT-3 GPS Data Assimilation on WRF model during 2007 Mei-yu season in Taiwan Shyuan-Ru Miaw, Pay-Liam Lin Department of Atmospheric Sciences.
Norman Weather Forecast Office Gabe Garfield 2/23/11.
Boundary layer depth verification system at NCEP M. Tsidulko, C. M. Tassone, J. McQueen, G. DiMego, and M. Ek 15th International Symposium for the Advancement.
Oct. 28 th th SRNWP, Bad Orb H.-S. Bauer, V. Wulfmeyer and F. Vandenberghe Comparison of different data assimilation techniques for a convective.
JCSDA Workshop Brock Burghardt August Model Configuration WRF-ARW v3.5.1 Forecasts integrated 30 hours Cycled every 6 hours (non-continuous boundaries)
Local Analysis and Prediction System (LAPS) Technology Transfer NOAA – Earth System Research Laboratory Steve Albers, Brent Shaw, and Ed Szoke LAPS Analyses.
August 6, 2001Presented to MIT/LL The LAPS “hot start” Initializing mesoscale forecast models with active cloud and precipitation processes Paul Schultz.
Low-level Wind Analysis and Prediction During B08FDP 2006 Juanzhen Sun and Mingxuan Chen Other contributors: Jim Wilson Rita Roberts Sue Dettling Yingchun.
STORM-SCALE DATA ASSIMILATION AND ENSEMBLE FORECASTING WITH THE NSSL EXPERIMENTAL WARN-ON-FORECAST SYSTEM 40 th National Weather Association Annual Meeting.
Local Analysis and Prediction System (LAPS) Technology Transfer NOAA – Earth System Research Laboratory Steve Albers, Brent Shaw, and Ed Szoke LAPS Analyses.
Brian Freitag 1 Udaysankar Nair 1 Yuling Wu – University of Alabama in Huntsville.
David H. Bromwich 1, 2 and Francis O. Otieno 1 1 Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, OH 2 Atmospheric.
15 June 2005RSA TIM – Boulder, CO Hot-Start with RSA Applications by Steve Albers.
WINDSOR TORNADO STUDY - STMAS (updated 10/21/2009 by Huiling Yuan and Yuanfu Xie)
Intelligent Use of LAPS • By • Ed Szoke • 16 May 2001.
National Weather Service Houston/Galveston Lance Wood Science and Operations Officer Assessing the Impact of MODIS SST Utilizing a local WRF.
WRF-based rapid updating cycling system of BMB(BJ-RUC) and its performance during the Olympic Games 2008 Min Chen, Shui-yong Fan, Jiqin Zhong Institute.
1 Recent AMDAR (MDCRS/ACARS) Activities at GSD New AMDAR-RUC database that helps evaluate AMDAR data quality Optimization study that suggests data can.
A. FY12-13 GIMPAP Project Proposal Title Page version 26 October 2011 Title: WRF Cloud and Moisture Verification with GOES Status: New GOES Utilization.
Rapid Update Cycle-RUC
Update on the Northwest Regional Modeling System 2013
NWS Forecast Office Assessment of GOES Sounder Atmospheric Instability
Winter storm forecast at 1-12 h range
Rapid Update Cycle-RUC Rapid Refresh-RR High Resolution Rapid Refresh-HRRR RTMA.
Junhua Zhang and Wanmin Gong
Real-time WRF EnKF 36km outer domain/4km nested domain D1 (36km)
NWP Strategy of DWD after 2006 GF XY DWD Feb-19.
Coastal Atmospheric Modeling for both Operational and Research Applications using the Weather Research Forecast (WRF) Model.
Start Hot-Start Section
Lightning Assimilation Techniques
Status of the Regional OSSE for Space-Based LIDAR Winds – Feb01
Presentation transcript:

Incorporation of TAMDAR into Real-time Local Modeling Tom Hultquist Science & Operations Officer NOAA/National Weather Service Marquette, MI

In a nutshell… Modeling system setup Modeling system setup Distribution of model output Distribution of model output Subjective impressions of model output Subjective impressions of model output Data deprivation experiments Data deprivation experiments Upcoming presentations Upcoming presentations Future work Future work

Modeling System FSL’s Local Analysis & Prediction System (LAPS), version used for data assimilation FSL’s Local Analysis & Prediction System (LAPS), version used for data assimilation Input data from MADIS & AWIPS netCDF files (METAR, RAOB, ACARS, Satellite, Maritime, Profiler, Mesonet, etc…) Input data from MADIS & AWIPS netCDF files (METAR, RAOB, ACARS, Satellite, Maritime, Profiler, Mesonet, etc…) LAPS is cycled hourly with WRF-ARW (v ), with 1- hour WRF-ARW forecast used as first guess in LAPS analysis (and subsequent LAPS analysis used to initialize WRF-ARW) LAPS is cycled hourly with WRF-ARW (v ), with 1- hour WRF-ARW forecast used as first guess in LAPS analysis (and subsequent LAPS analysis used to initialize WRF-ARW) Boundary conditions obtained from NAM (32 km files) Boundary conditions obtained from NAM (32 km files) 2 runs per day (03 UTC & 15 UTC) to 30 hours (hourly cycling restarted every 12 hours, using operational RUC for initial first guess) 2 runs per day (03 UTC & 15 UTC) to 30 hours (hourly cycling restarted every 12 hours, using operational RUC for initial first guess)

Modeling System Runs performed on dual processor Intel Xeon (3.3 GHz) workstation with 2 Gb RAM Runs performed on dual processor Intel Xeon (3.3 GHz) workstation with 2 Gb RAM Output from 30-hour simulations is available around 19 UTC (for 15 UTC run) and 07 UTC (for 03 UTC run) Output from 30-hour simulations is available around 19 UTC (for 15 UTC run) and 07 UTC (for 03 UTC run) Output from intermediate (cycled) runs and analyses is not currently made available Output from intermediate (cycled) runs and analyses is not currently made available

Modeling System 15 km grid spacing 15 km grid spacing 31 vertical layers 31 vertical layers 50 mb model top 50 mb model top KF convective scheme KF convective scheme Lin et al. microphysics Lin et al. microphysics RRTM longwave RRTM longwave Goddard shortwave Goddard shortwave Noah land surface model Noah land surface model YSU PBL YSU PBL

Model Output Output from the simulations is currently available at: Output from the simulations is currently available at: Output is in the form of RIP4 generated PNG images Output is in the form of RIP4 generated PNG images Output is hourly, with looping possible through javascript Output is hourly, with looping possible through javascript A variety of basic fields can be displayed as well as a few aviation specific fields and Skew-T diagrams for select locations A variety of basic fields can be displayed as well as a few aviation specific fields and Skew-T diagrams for select locations

Impressions Unable to perform any meaning objective verification Unable to perform any meaning objective verification Model output used somewhat frequently by local staff, but have received only minimal feedback from other offices (general consensus from SOOs is that forecasters are already overwhelmed with model output) Model output used somewhat frequently by local staff, but have received only minimal feedback from other offices (general consensus from SOOs is that forecasters are already overwhelmed with model output) Has been most useful in forecasting lack of convection (when operational models indicated convection) Has been most useful in forecasting lack of convection (when operational models indicated convection) Has also been useful in wind forecasts around Great Lakes Has also been useful in wind forecasts around Great Lakes LAPS balance routine often seems to remove detail/information which could prove useful LAPS balance routine often seems to remove detail/information which could prove useful

Data Deprivation Sought input from CR SOOs to help identify cases which could prove useful for data deprivation experiments Sought input from CR SOOs to help identify cases which could prove useful for data deprivation experiments Unfortunately, have received no recommendations, so only a few (locally identified) cases have be archived thus far Unfortunately, have received no recommendations, so only a few (locally identified) cases have be archived thus far Data from three cases has been archived, and these cases will be re- run identically, with the exception of TAMDAR data (which will be removed from one of the runs) Data from three cases has been archived, and these cases will be re- run identically, with the exception of TAMDAR data (which will be removed from one of the runs) February 27-28, 2005 – Significant winter storm and lake effect February 27-28, 2005 – Significant winter storm and lake effect June 24, 2005 – Non-event where real-time runs appeared to successfully capture overwhelming convective inhibition June 24, 2005 – Non-event where real-time runs appeared to successfully capture overwhelming convective inhibition August 9, 2005 – Widespread severe weather (bow echo) event in upper Michigan August 9, 2005 – Widespread severe weather (bow echo) event in upper Michigan Currently working on first case (preliminary results encouraging with regard to low track and placement of frontogenetically driven heavy snow band) ; Plan to complete these re-runs by early September Currently working on first case (preliminary results encouraging with regard to low track and placement of frontogenetically driven heavy snow band) ; Plan to complete these re-runs by early September Still interested in hearing about additional cases; A 14-day running archive is kept of all data, so cases can be “saved” within 2 weeks of their occurrence Still interested in hearing about additional cases; A 14-day running archive is kept of all data, so cases can be “saved” within 2 weeks of their occurrence

Sharing of Information Will present a summary of this TAMDAR modeling effort at the 14 th Annual U.S./Canada Great Lakes Operational Meteorology Workshop Will present a summary of this TAMDAR modeling effort at the 14 th Annual U.S./Canada Great Lakes Operational Meteorology Workshop Some information (particularly case examples) to be presented at the four NWS forecast offices in Michigan during this fall’s “traveling SOO show” in October Some information (particularly case examples) to be presented at the four NWS forecast offices in Michigan during this fall’s “traveling SOO show” in October

Future Work Try to get some additional cases identified Try to get some additional cases identified Possibly shrink domain and increase resolution of experiment prior to winter to better test performance during lake effect snow events Possibly shrink domain and increase resolution of experiment prior to winter to better test performance during lake effect snow events Update to latest versions of WRF-ARW and LAPS (should be able to get this done soon) Update to latest versions of WRF-ARW and LAPS (should be able to get this done soon) Cease local workstation Eta runs and replace with WRF-ARW (could allow for simultaneous runs with/without TAMDAR to provide real- time comparison) Cease local workstation Eta runs and replace with WRF-ARW (could allow for simultaneous runs with/without TAMDAR to provide real- time comparison)