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The 20101226 Blizzard Discussion1. Summary Discussion
a. Medium Range Issues (Days 4-7)b. Short-Range Issuesc. Ensemble trendsd. Upstream differences
2. Comments From Various Groups/Offices3. What To Do Next?
a. Science Goalsb. Operational Goals
CSTAR reference: http://dendrite.somas.stonybrook.edu/CSTAR/2627Dec2010.html
00 UTC 18 Dec Model Forecasts204 h forecast of 540 DM height valid 12 UTC 26 Dec
Courtesy: David Novak
12 UTC 22 Dec GFS ForecastWAVE PACKET EVOLUTION
http://ferrel.msrc.sunysb.edu/Wave/Dec22_12Z/F4-12hrly.htm
00 UTC 24 Dec Forecasts84 h forecast of 24 h accumulated precip
NAM GFS ECMWFCourtesy: David Novak
x NYC
Sensitivity of cyclogenesis to initial condition e.g., 03z, Dec. 24, 2010 SREF individual members (one Eta_KF and one RSM
members are very close to the observed)
Courtesy: Jun Du
Consequently, the problem for precipitation is that the major precipitation is too far from the coast prior to Dec. 25, 2010: e.g.
03z and 09z, Dec 24, 2010 SREF >1” (liquid equiv) probability
03z, 84hr 09z, 78hr
Courtesy: Jun Du and Rich Grumm
ETKF Sensitivity valid 27/1200 UTC
24/1200 UTCOne uncertainty areaNear Texas/Mexico
25/0000 UTCGrowing
Courtesy: Yucheng Song
26/0000 UTC
26/1200 UTC
Summary1. A Rossby wave packet led to downstream wave
amplification over NAmer., but the East Coast trough was underpredicted, especially > 3 days in advance.
2. The large shift in the models and ensembles between 0000 UTC 24 and 0000 UTC 25 Dec may have originated from small IC uncertainties/errors in the trough the central and southern central Plains.
3. Small IC differences between GFS and ECMWF at 1200 UTC 24 Dec amplified to large differences 36-48h later (GFS/GEFS appears to have done better than EC by ~12h).
4. Cyclone position was well forecast < 24-h but still mesoscale banding location issues (LI vs just west NYC).
5. Difference plots between models and run cycles is a useful tool. We need more of these plotting approaches in realtime to look at ensemble/model run to run differences.
Some Questions1. What led to the large change in GEFS solutions between
0000 and 1200 UTC 24 Dec?- previous model error finally corrected?- Important observations around SPlains?- Difficultly in trough (PV) merger?
2. Was there an impact of the targeted obs over the Gulf at 0000 UTC 25 December?
3. Why couldn’t ensemble (GEFS) perts over S. Plains create some cyclone solutions closer to obs for 24/00(06z) cycles? Why did the SREF cluster offshore as well?
4. Was there a large contribution from physics uncertainty in this event?
Future Plans for this Event• Look more carefully on how the predicted wave packets evolved in the medium range for this event using the TIGGE ensemble.• Use this case to test other metrics for ensemble sensitivity (see Edmund Chang presentation).• Look more carefully at what observations went into the 24/00z vs 24/12z cycles.• Need a web page to show difference plots from the various model and ensembles.• Others?