1 Localized Aviation Model Output Statistics Program (LAMP): Improvements to convective forecasts in response to user feedback Judy E. Ghirardelli National.

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Presentation transcript:

1 Localized Aviation Model Output Statistics Program (LAMP): Improvements to convective forecasts in response to user feedback Judy E. Ghirardelli National Weather Service Meteorological Development Laboratory October 11, 2011 “Friends/Partners in Aviation Weather” Forum NBAA Convention Las Vegas, NV

LAMP Background Statistical Guidance of sensible weather  Produced hourly, 25-h forecast period  Valid at stations (airports) and on a grid Elements of interest to Aviation: Winds (at stations) Ceiling height (at stations and gridded) Visibility (at stations and gridded) Thunderstorms (at stations and gridded) Visibility Thunderstorms Ceiling Height 2

How Did New LAMP Convection Guidance Evolve ? Existing Product: LAMP Lightning (LAMP ltg)  Predictand: ≥ 1 Cloud-to-Ground (CTG) lightning strike Review of existing practices to verify convection products (ESRL) indicates radar refl. of ≥ 40 dBZ used as indicator of “convection”  Problem: the verifying “truth” is not consistent with what LAMP lightning was intended to forecast FAA evaluation of operational LAMP ltg probabilities  Lacks spatial detail, skill, and sharpness especially beyond 6 hours MDL decisions (June 2010)  Define convection predictand:  radar ≥ 40 dBZ and/or ≥ 1 CTG lightning strikes  Add NAM MOS (to GFS MOS) convection probabilities as additional model input 3

Thunderstorm (current)Convection (future) 4 New LAMP Convective Guidance Features:  Defined from Cloud-to-Ground (CTG) ltg  GFS MOS 3-h thunderstorm probability predictors  2-h period / 20-km gridboxes  1-h cycle; 3 – 25 h projections  Other predictors Criticisms:  Convection can occur without CTG lightning  Thunderstorm probabilities lack sharpness Features:  Defined from CTG ltg / ≥ 40 dBZ radar reflectivity  GFS & NAM MOS 2-h convective probability predictors  2-h period / 20-km gridboxes  1-h cycle; 3 – 25 h projections  Other predictors Solution:  Convection can be indicated when there is little or no lightning  Convection probabilities exhibit good sharpness

5 Convection Potential Four convection potential categories  No, low, medium, and high  Each category is defined objectively from a pre-determined probability threshold  Each probability threshold corresponds to a prescribed bias criterion, where bias is  ~ 2.7 = low potential  ~ 1.1 = medium potential (lightning ~ 1.2)  ~ 0.4 = high potential Convection potential aids interpretation of probabilities with peak values < 100%

6 LAMP Lightning (LTG) vs Convection(CNV) Prob. Skill for 1800 UTC Cycle Cool seasonSpring season Summer season Independent sample Oct 2009 – Oct 2010

7 LAMP Lightning vs Convection Probability Reliability and Sharpness

New LAMP Convective Guidance 8 August 27, 2011: 1800 UTC cycle, Hurricane Irene LAMP LightningLAMP Convection

New LAMP Convective Guidance 9 Convection Probabilities Convection Potential August 25, 2011: 1200 UTC cycle, 6-8 hour projection

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12 Note that this is a 23-hour projection, and the LAMP convective probabilities are about 90% while the LAMP thunderstorm probabilities are about 30%.

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14 May 26, 2011: 0000 UTC cycle: Chicago, Atlanta, New York all affected Convective Guidance Examples

15 Convective Guidance Examples September 07, 2011: 0000 UTC cycle

16 September 07, 2011: 0000 UTC cycle: hour projection Convective Guidance Examples

Future Work: Additional Products 17 Verification Graphics: overlay probabilities with marker indicating if convection was observed Text bulletins at stations: to support prototype Gate Forecasts

Implementation Plans Convection products produced in real time since March 2011  24 cycles per day (not supported 24x7)  Web Graphics at:  GRIB2 files available at: Implement on CCS parallel system before March 2012 Available in experimental NDGD March 2012 Transmit grids on SBN/NOAAPORT – planned FY12/13 Contact: 18