NCEP Model Comparisons over the East and West Coast of the US Lynn McMurdie Garrett Wedam Cliff Mass May 27, 2009 Wedam, McMurdie and Mass, 2009: Comparison.

Slides:



Advertisements
Similar presentations
ECMWF Training Course 2005 slide 1 Forecast sensitivity to Observation Carla Cardinali.
Advertisements

Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at.
ECMWF long range forecast systems
CanSISE East meeting, CIS, 10 February 2014 Seasonal forecast skill of Arctic sea ice area Michael Sigmond (CCCma) Sigmond, M., J. Fyfe, G. Flato, V. Kharin,
94th American Meteorological Society Annual Meeting
2007 AEW activity in Global models. - Following Berry, Thorncroft and Hewson (2007; henceforth BTH07) we use 700hPa wind to compute curvature, shear vorticity.
My Agenda for CFS Diagnostics Ancient Chinese proverb: “ Even a 9-month forecast begins with a single time step.” --Hua-Lu Pan.
Convection-permitting forecasts initialized with continuously-cycling limited-area 3DVAR, EnKF and “hybrid” data assimilation systems Craig Schwartz and.
Using ensemble data assimilation to investigate the initial condition sensitivity of Western Pacific extratropical transitions Ryan D. Torn University.
Review of Northern Winter 2010/11
An Investigation of Cool Season Extratropical Cyclone Forecast Errors Within Operational Models Brian A. Colle 1 and Michael Charles 1,2 1 School of Marine.
Real-time WRF EnKF 36km outer domain/4km nested domain 36km outer domain/4km nested domain D1 (36km) D2 (4km)
East Coast vs. West Coast: A Documentation of Model Forecast Failures for Eta, NAM, GFS, GEM, and ECMWF Garrett Wedam Lynn McMurdie, Cliff Mass.
Brian Ancell, Cliff Mass, Gregory J. Hakim University of Washington
United States Coast Guard 1985 Evaluation of a Multi-Model Storm Surge Ensemble for the New York Metropolitan Region Brian A. Colle Tom Di Liberto Stony.
GFS (left), ECMWF (right) 500 mb Height, Winds, and Temp 00 hr forecast valid 12z 24 Dec 2010.
GFS (green), ECMWF (blue) 500 mb height 00 hr forecasts 12z 24 Dec
The Blizzard Discussion 1.Summary Discussion a. Medium Range Issues (Days 4-7) b. Short-Range Issues c. Ensemble trends d. Upstream differences.
Ensemble Post-Processing and it’s Potential Benefits for the Operational Forecaster Michael Erickson and Brian A. Colle School of Marine and Atmospheric.
GDAS analysis 500 mb height/absolute vorticity 00z 24 Dec 2010.
Consolidated Seasonal Rainfall Guidance for Africa Dec 2012 Initial Conditions Summary Forecast maps Forecast Background – ENSO update – Current State.
Ensemble storm surge forecasting in the UK during the exceptional 2013/14 winter Helen Titley Senior Weather Impacts Scientist, Met Office, UK With thanks.
ECMWF Training Course 2005 slide 1 Forecast sensitivity to Observation Carla Cardinali.
Forecast Skill and Major Forecast Failures over the Northeastern Pacific and Western North America Lynn McMurdie and Cliff Mass University of Washington.
Observing Strategy and Observation Targeting for Tropical Cyclones Using Ensemble-Based Sensitivity Analysis and Data Assimilation Chen, Deng-Shun 3 Dec,
National Weather Service Model Flip-Flops and Forecast Opportunities Bernard N. Meisner Scientific Services Division NWS Southern Region Fort Worth, Texas.
1 AMDAR Quality Assurance Bradley Ballish NOAA/NWS/NCEP/NCO/PMB SSMC2/Silver Spring 23 March, 2009.
NARCCAP Users Meeting April 2011 Results from NCEP-driven RCMs Overview Based on Mearns et al. (BAMS, 2011) Results from NCEP-driven RCMs Overview Based.
Eidgenössisches Departement des Innern EDI Bundesamt für Meteorologie und Klimatologie MeteoSchweiz Statistical Characteristics of High- Resolution COSMO.
Impact of Targeted Dropsonde Data on Mid-latitude Numerical Weather Forecasts during the 2011 Winter Storms Reconnaissance Program Presented by Tom Hamill.
On Improving GFS Forecast Skills in the Southern Hemisphere: Ideas and Preliminary Results Fanglin Yang Andrew Collard, Russ Treadon, John Derber NCEP-EMC.
Forecast Pressure. Pressure Observations ASOS is the best…the gold standard Ships generally the worst.
The African Monsoon Recent Evolution and Current Status Update prepared by Climate Prediction Center / NCEP 6 December 2010 For more information, visit:
Consolidated Seasonal Rainfall Guidance for Africa, Jan 2013 Initial Conditions Summary Forecast maps Forecast Background – ENSO update – Current State.
Model validation Simon Mason Seasonal Forecasting Using the Climate Predictability Tool Bangkok, Thailand, 12 – 16 January 2015.
1 Rolf Langland Naval Research Laboratory – Monterey, CA Uncertainty in Operational Atmospheric Analyses.
Modification of GFS Land Surface Model Parameters to Mitigate the Near- Surface Cold and Wet Bias in the Midwest CONUS: Analysis of Parallel Test Results.
1 Discussion of Observational Biases of Some Aircraft Types at NCEP Dr. Bradley Ballish NCEP/NCO/PMB 7 September 2006 “Where America’s Climate and Weather.
The South American Monsoon System: Recent Evolution and Current Status Update prepared by Climate Prediction Center / NCEP 30 December 2013 For more information,
Verification of Global Ensemble Forecasts Fanglin Yang Yuejian Zhu, Glenn White, John Derber Environmental Modeling Center National Centers for Environmental.
Ensemble-based prediction and diagnostics during the PREDICT field experiment Sharan Majumdar (RSMAS / U. Miami) Ryan Torn (SUNY at Albany) Fuqing Zhang.
1 Results from Winter Storm Reconnaissance Program 2007 Yucheng SongIMSG/EMC/NCEP Zoltan TothEMC/NCEP/NWS Sharan MajumdarUniv. of Miami Mark ShirleyNCO/NCEP/NWS.
Application of Numerical Weather Prediction Prognoses to Operational Weather Forecasting in Hong Kong Pre-CAS Technical Conference on "Environmental Prediction.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss TECO-2006, WMO, Geneva, Global Criteria for.
Development Mechanism of Heavy Rainfall over Gangneung Associated with Typhoon RUSA Tae-Young Lee, Nam-San Cho, Ji-Sun Kang Kun-Young Byun, Sang Hun Park.
Overview of 2012/2013 winter over South Korea
Assess Observation Impacts in the Hybrid GSI-EnKF Data Assimilation Systems for NCEP Global Forecast System Model Through OSE and Ensemble Based Observation.
Predictability of High Impact Weather during the Cool Season: CSTAR Update and the Development of a New Ensemble Sensitivity Tool for the Forecaster Brian.
Exploring Multi-Model Ensemble Performance in Extratropical Cyclones over Eastern North America and the Western Atlantic Ocean Nathan Korfe and Brian A.
Transitioning unique NASA data and research technologies to the NWS 1 AIRS Data Assimilation at SPoRT Brad Zavodsky and Will McCarty (UAH) Shih-hung Chou.
- 200 hPa geopotential heights in the GDAS analysis are lower than in CDAS between 20 o N to the South Pole hPa geopotential heights are consistently.
- 200 hPa geopotential heights in the GDAS analysis are lower than in CDAS between 20 o N to the South Pole hPa geopotential heights are consistently.
Quantifying the Significance of the April 2011 Severe Weather Outbreak Matthew S. Stalley, Chad M. Gravelle, Charles E. Graves Saint Louis University.
Optimization Of Sun-synchronous Orbital Planes; activities in the United States Lars Peter Riishojgaard Director, Joint Center for Satellite Data Assimilation.
NCEP CMC ECMWF MEAN ANA BRIAN A COLLE MINGHUA ZHENG │ EDMUND K. CHANG Applying Fuzzy Clustering Analysis to Assess Uncertainty and Ensemble System Performance.
10th COSMO General Meeting, Cracow, Poland Verification of COSMOGR Over Greece 10 th COSMO General Meeting Cracow, Poland.
NCEP Dropout Team Briefing JAG/ODAA Meeting OFCM October 2008 “Where America’s Climate, Weather and Ocean Prediction Services Begin” Jordan Alpert, Bradley.
Forecast Pressure. Pressure Observations ASOS is the best…the gold standard Ships generally the worst.
NASA, CGMS-44, 7 June 2016 Coordination Group for Meteorological Satellites - CGMS SURFACE PRESSURE MEASUREMENTS FROM THE ORBITING CARBON OBSERVATORY-2.
The impact of lower boundary forcings (sea surface temperature) on inter-annual variability of climate K.-T. Cheng and R.-Y. Tzeng Dept. of Atmos. Sci.
© Crown copyright Met Office Review topic – Impact of High-Resolution Data Assimilation Bruce Macpherson, Christoph Schraff, Claude Fischer EWGLAM, 2009.
Station lists and bias corrections Jemma Davie, Colin Parrett, Richard Renshaw, Peter Jermey © Crown Copyright 2012 Source: Met Office© Crown copyright.
Weather Regimes and Forecast Errors in the Pacific Northwest Lynn McMurdie (co-author Joe Casola) University of Washington.
WRF-EnKF Lightning Assimilation Real-Observation Experiments Overview
An Analysis of Large Track Error North Atlantic Tropical Cyclones.
Forecast Pressure.
Forecast Pressure.
WP4.1 : Exploiting CCI products in CMIP like experiments
Forecast Pressure.
Forecast Pressure.
Presentation transcript:

NCEP Model Comparisons over the East and West Coast of the US Lynn McMurdie Garrett Wedam Cliff Mass May 27, 2009 Wedam, McMurdie and Mass, 2009: Comparison of Model Forecast Skill of Sea-level Pressure along the East and West Coasts of the United States. Wea. Forecasting, 24,

Large Short-term forecast errors can still occur despite recent model improvements NCEP NAM 72-h forecasts (white), analyses (black), slp errors (black numbers) valid on 0000 UTC 24 December NCEP GFS 72-h forecast (cyan) and slp errors (black numbers) valid 1200 UTC 1 January 2009

Goals Document the frequency and magnitude of sea level pressure forecast errors Compare the accuracy of several operational (deterministic) numerical model systems Compare the accuracy of forecasts along the East and West Coasts of the US Examine preliminary results from the past winter (2008 – 2009)

Methods -- Observations Used buoys and c-man observations along the east and west coast. Observed SLP variance was calculated and west and east coast buoys were matched if they had the same 30-day variance – 11 pairs total For each model and forecast hour, an average error (Coastal Mean Absolute Error, CAE) was calculated for every forecast cycle. These CAE’s were then averaged for each month. Also calculated the large-error frequency (number of forecasts exceeding a large-error criteria)

Buoys matched by variance Compare results for the ECMWF, CMC-GEM and NCEP GFS and NAM models for three winter seasons: Nov 2005– Mar 2006, Nov 2006 – Mar 2007, Nov 2007 – Mar 2008.

ECMWF has smaller errors than other models for most months. NAM has larger errors than other models for most months and forecast hrs. Coastal Mean Absolute Error for all models, forecast hours and both coasts NAM upgrade to WRF-NMM

East Coast errors smaller than West Coast errors for all months and forecast hours Coastal Mean Absolute Error for all models, forecast hours and both coasts

Histograms of f48 Errors

Frequency of Large Errors >3hPa >5hPa >7hPa Same conclusions apply: ECMWF smallest frequency and NAM the largest frequency of large errors, East Coast smaller frequency of large errors than West Coast for all models and forecast hours.

Have any models shown improvement over the course of the study? ECMWF improved GFS improved West Coast CMCG improved second year NAM ?? Anomaly CAE = 3-season CAE minus individual season CAE

Did the data assimilation upgrade in Dec 2008 improve forecasts of SLP for the NAM? Assimilation upgrade Dec 2008 NAM forecast errors much larger than GFS errors NAM forecast errors NOT significantly larger than GFS “Background for the first analysis is from the GDAS instead of the previous NDAS”

Summary The West Coast has larger and more frequent SLP forecast errors than the East Coast. The NAM consistently underperformed and the ECMWF outperformed all the other models in the study Preliminary results from this past winter ( ) show that the data assimilation upgrade has improved SLP forecasts for the NAM model