AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction - 2007 – Park City, Utah 1 June 26, 2007 EVALUATION.

Slides:



Advertisements
Similar presentations
Historic Winter Storm/Blizzard February 8-9, 2013 Historic Winter Storm/Blizzard February 8-9, 2013 Updated Headlines: 4 PM Thursday, February 7 th, 2013.
Advertisements

Summer 2009 Western Fire Season Outlook Overview Significant fire potential is expected to be above normal across much of California, Florida, central.
On December 1, 1913, a low-pressure system developed over northern Arizona, bringing precipitation to most of Eastern Colorado. What followed over the.
Jess Charba Fred Samplatsky Phil Shafer Meteorological Development Laboratory National Weather Service, NOAA Updated September 06, 2013 LAMP Convection.
Characteristics of Upslope Snowfall Events in Northern New York State and Northern Vermont Diagnostics and Model Simulations of Several Northwest-Flow.
GROUP 4 : UPDATED 22 Feb 2007 Huigang Yang Wendi Kaufeld Matt Sienko.
Louisville, KY August 4, 2009 Flash Flood Frank Pereira NOAA/NWS/NCEP/Hydrometeorological Prediction Center.
Met Brief, Lenny Pfister Nick Heath. Weather today/yesterday.
Holly A. Anderson Spring 2007 – Synoptic II Florida State University Introduction On December 10, 1995, Buffalo, New York experienced a record-breaking.
NOAA/NWS Change to WRF 13 June What’s Happening? WRF replaces the eta as the NAM –NAM is the North American Mesoscale “timeslot” or “Model Run”
National Weather Service – Reno Northern Nevada 2015 Streamflow Forecast Meeting Mar 20, 2015.
Chapter 9: Weather Forecasting Acquisition of weather information Acquisition of weather information Weather forecasting tools Weather forecasting tools.
A Compare and Contrast Study of Two Banded Snow Storms Part I – January 6 th, 2002.
Forecast Challenges Associated with the Valentine’s Day, St. Patrick’s Day and Tax Day Nor’easters of 2007 Neil A. Stuart NWS Albany, NY NROW 9.
FORECASTING EASTERN US WINTER STORMS Are We Getting Better and Why? Jeff S. Waldstreicher NOAA/NWS Eastern Region Scientific Services Division – Bohemia,
The March 01/02 Non-Winter Weather Event: Part 1 Michael W. Cammarata Anthony W. Petrolito.
Ryan Ellis NOAA/NWS Raleigh, NC.  The development of orographically induced cirrus clouds east of the southern Appalachian Mountain chain can result.
ATOC 6700 Weather Forecasting Discussion. Student Introductions Tell us: – Your name – Your year in ATOC graduate program – The topic of your research.
Radar Animation 9:30 AM – 7:00 PM CST November 10, 2006 …Excerpt from Meteorological Overview of the November 10, 2006 Winter Storm… Illustrate value of.
TAMDAR Alaskan data compiled by Ed Szoke NOAA/CIRA/GSD 2007 cases comparing TAMDAR out of Anchorage (ANC) and other Alaska airports nearby RAOB cases Airports.
Model Verification of Short Range High Impact Weather in Central Florida Christopher Hicks Department of Marine and Environmental Systems Florida Institute.
Kristopher White & Brian Guyer The GOES-R Convective Initiation Product... Operational Examples and Thoughts on Proper Viewing Strategies.
Use of TAMDAR Data in a Convective Weather Event Saturday, May 21, 2005.
GROUP # 5 UPDATED 02/20/07 Faye Barthold Michelle Benny Ting Sun.
Phillip Bothwell Senior Development Meteorologist-Storm Prediction Center 3 rd Annual GOES-R GLM Science Meeting Dec. 1, 2010 Applying the Perfect Prog.
Forecasting and Numerical Weather Prediction (NWP) NOWcasting Description of atmospheric models Specific Models Types of variables and how to determine.
Poorly Forecast Convection During the Evening of 20 July 2008 in Southern North Dakota Justin Turcotte Meteorologist Meridian Environmental Technology.
Hurricane lecture for KMA Ed Szoke 1 October 20, 2004 Overview of 2004 Atlantic Hurricane Season Ed Szoke* NOAA Forecast Systems Laboratory Forecast Research.
Poster 1.66 An Update on CIRA’s GOES-R Proving Ground Activities Ed Szoke 1,2, Renate Brummer 1, Hiro Gosden 1, Steve Miller 1, Mark DeMaria 3, Dan Lindsey.
Week in Review 8/28/13 to 9/4/13 John Cassano. Weather Situation – Strong upper level ridge over central US – Jet stream well north of US – Weak frontal.
MDSS Lab Prototype: Program Update and Highlights Bill Mahoney National Center For Atmospheric Research (NCAR) MDSS Stakeholder Meeting Boulder, CO 20.
Special Winter Weather Briefing 2/3/2011 – 4 PM slides: Keith Stellman National Weather Service Shreveport, Louisiana.
Ming Hu Developmental Testbed Center Introduction to Practice Session 2011 GSI Community Tutorial June 29-July 1, 2011, Boulder, CO.
1 Appendix. 2 For the Encore: NYC Blizzard (Dec 25-27, 2010)
Higher Resolution Operational Models. Operational Mesoscale Model History Early: LFM, NGM (history) Eta (mainly history) MM5: Still used by some, but.
AMS 23 rd Conference on Severe Local Storms/2006 – St. Louis Talk November 8, 2006 AN EVALUATION OF TAMDAR SOUNDINGS IN SEVERE WEATHER FORECASTING.
Ensemble Forecasting and You The very basics Richard H. Grumm National Weather Service State College PA
An Experiment to Evaluate the Use of Quantitative Precipitation Forecasts from Numerical Guidance by Operational Forecasters Joshua M. Boustead and Daniel.
TAMDAR Workshop 2006 – Boulder, Colorado 1 April 13, 2006 UPDATE ON TAMDAR IMPACT ON RUC FORECASTS & RECENT TAMDAR/RAOB COMPARISONS Ed Szoke,* Brian Jamison*,
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.
Performance of the Experimental 4.5 km WRF-NMM Model During Recent Severe Weather Outbreaks Steven Weiss, John Kain, David Bright, Matthew Pyle, Zavisa.
NATS 101 Section 6: Lecture 3 Weather vs. Climate.
Other Factors: Bias of Forecasting Models “The GFS (Global Forecast Index) is a U.S. based model that can extend out 384 hours or to about Christmas Eve.
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.
AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 1 June 26, 2007 IMPACT.
Ed Szoke 1 April 12, 2005 TAMDAR Project – April Boulder Meeting Ed Szoke* NOAA Forecast Systems Laboratory *Joint collaboration with the Cooperative Institute.
MMET Team Michelle Harrold Tracy Hertneky Jamie Wolff Demonstrating the utility of the Mesoscale Model Evaluation Testbed (MMET)
Boulder TAMDAR Meeting - Ed Szoke 1 August 25, 2005 RUC – RAOB – TAMDAR SOUNDINGS Ed Szoke* NOAA Forecast Systems Laboratory *Joint collaboration with.
Heavy snow impacted Italy and the Balkans with record snows on both sides of the Adriatic ” of snow fell in 18 hours. Pescocostanzo, Italy – 21 miles.
Bay Effect Snow from the Chesapeake Bay David F. Hamrick WPC Meteorologist College Park, Maryland.
Model Jumpiness and the Need for Ensembles Richard Grumm National Weather Service Office and Lance Bosart State Univesity of New York at Albany Richard.
Briefing, , conditions Monday/Tuesday Aug 5/6 Chance of some thin cirrus off NORCAL coast today Models have backed off on the cirrus forecast for.
Northeast/AWT Widespread rains from 7 Dec 2011 Slow-moving surface low eventually accelerated through the Northeast Some heavy rainfall, particularly after.
Do the NAM and GFS have displacement biases in their MCS forecasts? Charles Yost Russ Schumacher Department of Atmospheric Sciences Texas A&M University.
HWT Spring Experiment 2011 model comparisons 1 June OK-MO severe storms Very subtle boundaries, really not a lot of surface forcing But lots of storms.
ATOC 6700 Weather Forecasting Discussion. THIS CLASS IS NOT ABOUT WEATHER FORECASTING.
Met Brief, Lenny Pfister Nick Heath. Outline Tomorrow’s flight – Convection – Surface temperatures – Convective outflow Friday’s flight – East.
AMS 13 th Conference on Aviation, Range and Aerospace Meteorology – January 2008 – New Orleans, Louisiana 1 January 22, 2008 EFFECT OF TAMDAR ON RUC SHORT-TERM.
STMAS (Aviation Weather Testbed (AWT-2011) case: 22 July 2011 Highlight: Strong storms with a small line move through Chicago (O’Hare Airport) at 15z with.
Optimization Of Sun-synchronous Orbital Planes; activities in the United States Lars Peter Riishojgaard Director, Joint Center for Satellite Data Assimilation.
Estimating Potential Impacts of Climate Change on the Park City Ski Area Brian Lazar Stratus Consulting Inc. Mark Williams.
Brian Freitag 1 Udaysankar Nair 1 Yuling Wu – University of Alabama in Huntsville.
National Weather Service Houston/Galveston Lance Wood Science and Operations Officer Assessing the Impact of MODIS SST Utilizing a local WRF.
Grupo de Meteorologia e Climatologia na Universidade de Aveiro Alfredo Rocha, Tiago Luna, Juan Ferreira, Ana Carvalho and João.
AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 1 June 26, 2007 IMPACT.
A Possible Relationship Between Total Lightning and Non-Supercell Tornadogenesis Ed Szoke1,2, Dan Bikos1, Geoffrey Stano3, Pat Kennedy4, Steve Rutledge4,
The November 26, 2014 banded snowfall case in southern NY
Communicating Uncertainty via Probabilistic Forecasts for the January 2016 Blizzard in Southern New England Frank M Nocera, Stephanie L. Dunten & Kevin.
Update on the Northwest Regional Modeling System 2017
452 Precipitation.
Presentation transcript:

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 1 June 26, 2007 EVALUATION OF THE NCEP WRF NMM AND ARW MODELS FOR SOME RECENT HIGH-IMPACT WEATHER EVENTS Ed Szoke 1,2, Steve Koch 2, Dave Barjenbruch 3, and Doug Wesley 4 2 NOAA/Earth Systems Research Laboratory Global Systems Division 1 Joint collaboration with the Cooperative Institute for Research in the Atmosphere, Colorado State University, Fort Collins, CO 3 NOAA National Weather Service, Boulder, Colorado 4 Cooperative Program for Operational Meteorology, Education and Training (COMET), Boulder, Colorado

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 2 June 26, 2007 Overview At the last WAF/NWP Conference in D.C. (August/2005) there was a session with talks on the DWFE (DTC Winter Forecast Experiment) and the high-resolution models run during DWFE During that session Nelson Seaman announced that NCEP would begin to routinely run hi-res windows for the ARW and NMM at ~5 km horizontal grid resolution, in part because of the DWFE experience Since late 2005 these runs have been made in real-time and posted to the web Purpose of this talk Examine the hi-res models for some recent winter high-impact events Compare to the operational models (NAM and GFS) Focus on precipitation forecasts Do the hi-res models offer improved guidance to the forecaster for these events? In this talk will focus on the big pre-Christmas 2006 blizzard in Colorado

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 3 June 26, 2007 Coverage and initialization times for the high-resolution window runs

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 4 June 26, 2007 Run out to: 84 h 240 h 48 h

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 5 June 26, 2007 Headlines on Thursday 21 December 2006 (Denver Post)

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 6 June 26, 2007 Headlines on Friday 22 December 2006 (Denver Post)

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 7 June 26, 2007 Boulder Daily Camera headline on Thursday 21 December. For some, a 15 min commute turned into 2+ hours. Others were stranded...

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 8 June 26, 2007 Midday 20 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 9 June 26, 2007 Late in the day 20 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 10 June 26, 2007 The next morning ” total

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 11 June 26, 2007 This storm was followed by another foot+ storm the next week...scene by 30 Dec 06

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 12 June 26, 2007 The focus today will be on the first storm...snow totals: max 50” in the foothills west of Fort Collins, ~20-24” Denver city

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 13 June 26, 2007 Statistics Terrain is a big player in modulating snowfall...

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 14 June 26, 2007 Estimated precipitation totals from the NOHRSC. Max totals for 24 h ending: 0600 UTC/21 Dec = ” 0600 UTC/22 Dec = ” totals ~ 2-2.8” For comparison with model forecasts need precipitation totals. Most of the snow fell from 1200 UTC/20 Dec to 1200 UTC/21 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 15 June 26, 2007 Note the minimum downstream of the Cheyenne Ridge of ” Agrees pretty much with the Boulder NWS estimated total precip using many volunteer and official reports

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 16 June 26, 2007 This was a high-impact event for areas well-beyond Northeast Colorado Watches and warnings as of 0000 UTC 20 December

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 17 June 26, mb analysis: 1200 UTC/18 Dec 2006

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 18 June 26, mb analysis: 1200 UTC/19 Dec 2006

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 19 June 26, mb analysis: 1200 UTC/20 Dec 2006

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 20 June 26, mb analysis: 0000 UTC/21 Dec 2006

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 21 June 26, 2007 Statistics Time 1: 1200 UTC 18 Dec GFS 48-h 700 mb forecast valid 1200 UTC/20 Dec Elongated upper-low with nw flow along Front Range.

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 22 June 26, 2007 Similar to GFS 18 Dec 06/1200 UTC NAM 48 h 700 mb valid 1200 UTC 20 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 23 June 26, 2007 Also an elongated low, but more N to NNE flow along the Front Range 18 Dec 06/1200 UTC WRF/ARW 48 h 700 mb valid 1200 UTC 20 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 24 June 26, 2007 flow is even more NE at ~10 kts with hint of secondary low 18 Dec 06/1200 UTC WRF/NMM 48 h 700 mb valid 1200 UTC 20 Dec Big picture is similar to the GFS and NAM... but along the Front Range

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 25 June 26, 2007 Much more circular 700 mb low is what verifies Verifying 700 mb analysis at 20 Dec 06/1200 UTC

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 26 June 26, 2007 Deep upslope just above 700 mb. 20 Dec 06/1200 UTC Denver sounding

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 27 June 26, 2007 Results in lots of snow wrapping into Colorado UTC/20 Dec radar.

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 28 June 26, 2007 Much better 700 mb shape and location of the upper low but flow is still too northerly Time 2: 19 Dec 06/0600 UTC GFS 42-h 700 mb valid 0000 UTC 21 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 29 June 26, 2007 Somewhat better flow tho still nw at ~ Denver's location 19 Dec 06/0600 UTC NAM 42 h 700 mb forecast valid 0000 UTC 21 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 30 June 26, 2007 Flow is more NNE and strong (30 kts) near Denver 19 Dec 06/0600 UTC WRF/ARW 42 h 700 mb forecast valid 0000 UTC 21 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 31 June 26, 2007 Pretty close to the ARW 19 Dec 06/0600 UTC WRF/NMM 42-h 700 mb forecast valid 0000 UTC 21 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 32 June 26, 2007 Upper low is deepening in a perfect spot Verifying 700 mb analysis at 21 Dec 06/0000 UTC

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 33 June 26, 2007 Deep northeast flow. Evidence of low level damming with a more nw surface wind. 21 Dec 06/0000 UTC Denver sounding

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 34 June 26, 2007 The more N to NW flow forecast for the Front Range kept precip amounts too low near the foothills/Urban Corridor. 19 Dec 06/0600 UTC GFS 48 h total precipitation ending 0600 UTC 21 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 35 June 26, 2007 NAM had better NE flow at least in northern CO so better wrap-around precip, but not far enough south so Denver kept out of the heavy amounts. 19 Dec 06/0600 UTC NAM 48 h total precipitation ending 0600 UTC 21 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 36 June 26, 2007 Not so with the ARW. Denver is located near the “X”, with 2-2.5” predicted just to the nw. Note the minimum of precip in the ” range downstream of the Cheyenne Ridge. Also a good forecast of the heavier precip extending east of Denver near 40 o N. 19 Dec 06/0600 UTC WRF/ARW 48 h total precipitation ending 0600 UTC 21 Dec x min 40 o N

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 37 June 26, 2007 NMM also has great wrap-around precip all the way to Denver, though not as much as the ARW (max amounts in this forecast in the ” range). Also a min downstream of the Cheyenne Ridge but not as dramatic ( ”) as in the ARW forecast. 19 Dec 06/0600 UTC WRF/ARW 48 h total precipitation ending 0600 UTC 21 Dec x x min

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 38 June 26, 2007 Precipitation analysis (repeated)

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 39 June 26, mb forecasts were similar for this final time (~ 6-8 h before the S+ began), so will only show the precipitation forecasts. GFS still having trouble getting the max amounts back into the Front Range but is better, with 1.26” max near Fort Collins. Time 3: 20 Dec 06/0600 UTC GFS 48 h total precipitation ending 0600 UTC 22 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 40 June 26, 2007 NAM is much better. Max is now just over 3”. Also, nicely picks up the min south of the Cheyenne Ridge (of ”) as well as a min south of the Palmer Ridge (near Colorado Springs, similar) Observed amounts in the Springs area were as low as just under 0.5”. 20 Dec 06/0600 UTC NAM 48 h total precipitation ending 0600 UTC 22 Dec

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 41 June 26, 2007 Max amounts now up to the 3-4” range just w-nw of Denver (marked by X). The mins south of the Cheyenne Ridge and the Palmer Divide are similar to those forecast by the NAM. 20 Dec 06/0600 UTC WRF/ARW 48 h total precipitation ending 0600 UTC 22 Dec x

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 42 June 26, 2007 Similar forecast to the ARW, except a little less precip east of Denver. 20 Dec 06/0600 UTC WRF/NMM 48 h total precipitation ending 0600 UTC 22 Dec x

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 43 June 26, 2007 Summary of the big storm Early forecasts ~ 48 h in advance of the storm were similar on the larger scale with an elongated 700 mb low in all the models But the high-resolution runs had more favorable flow near the Front Range...is this a result of the flow modeled at higher resolution interacting with higher resolution terrain? The higher resolution models had better precipitation forecasts sooner than the operational models, with the GFS slowest to come around to having the precipitation wrap into the Front Range. Close to the storm onset the NAM forecast was fairly similar to that from the high resolution models Including being able to capture precipitation minima and maxima that were highly modulated by terrain Forecasts from the ARW and NMM were relatively close...a little more precipitation from the ARW. For this case the precipitation amounts forecast from the high-resolution models were in line with observed totals. More generally, we have noticed a tendency to over predict orographic precipitation, especially with weaker synoptic systems.

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 44 June 26, 2007 Some thoughts on the high-resolution runs The runs were accessible through the web (for the most part). Are they being used? An informal survey of several WFOs suggested they are not used much. Why? Not on AWIPS (also, therefore, cannot input to IFPS) Run only once per day (although depending where you are, like in Colorado, two windows overlap) so model output becomes “old” compared to the six-hourly operational runs Model forecast reflectivity was a very popular product during DWFE, but was not available on the web The future looks better! NCEP plans to make changes: Bigger, CONUS sized windows Run twice daily At 4 km horizontal grid resolution With attempt to get output into AWIPS

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 45 June 26, 2007 Here is an event that was a big bust for the Front Range. 48-h 700 mb forecast from the NAM valid at 1200 UTC 13 April Note the upslope flow in the forecast. Lastly....if the NAM has a really bad forecast, the high-resolution model will also go down

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 46 June 26, mb low verifies farther west and south...no upslope for Denver/Boulder!

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 47 June 26, 2007 As a result most of the precipitation stayed to the south

AMS 22 nd Conference on Weather Analysis and Forecasting/18 th Conference on Numerical Weather Prediction – Park City, Utah 48 June 26, 2007 Somewhat different forecasts for northeastern Colorado, but both models predict too much precipitation too far north (really nothing verified in southeast Wyoming). 48-h total precipitation forecasts from the hi-res models ending at 1200 UTC 31 April ARW NMM