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Probabilistic Lightning Forecasts Using Deterministic Data. Evan Kuchera and Scott Rentschler 16 Aug 2007. Motivation. Air Force operators require skillful and objective probabilistic weather information to maximize efficiency and minimize loss - PowerPoint PPT Presentation
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I n t e g r i t y - S e r v i c e - E x c e l l e n c e
Air Force Weather Agency
Probabilistic Lightning Forecasts Using Deterministic
Data
Evan Kuchera and Scott Rentschler16 Aug 2007
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Motivation
Air Force operators require skillful and objective probabilistic weather information to maximize efficiency and minimize loss
Typically this is accomplished with ensembles for grid scale phenomena
However, sub grid scale processes are probabilistic in nature even with deterministic data
We believe that ensemble forecast skill will be higher if a probabilistic approach is taken with each ensemble member for sub grid scale phenomena Addresses both sub-grid scale and flow uncertainties
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Motivation
Example—lightning forecast with SPC SREF method 10 ensemble members CAPE values of 130,125,120,115,110,105,103,102,101,101
With a forecast threshold of 100 J/kg, this gives a 100% chance of lightning
However, with values so close to the threshold, the true probability is likely much closer to 50% than 100%
This can be accounted for somewhat with real-time calibration after the ensemble is created (as SPC does with success), but this is not necessarily an option for the Air Force (resource constraints, lack of calibration data)
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Background
Lightning background: Need graupel and ice particle collisions to transfer
negative charge to the larger particles Thunderstorm updrafts need to grow large graupel
particles with enough fall speed to cause a separation of charge in the vertical
The theoretical value of CAPE required to do this is only 25 J/kg
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Background
CAPE background: Accepted parcel theory assumption is that as the parcel
rises, all condensate is immediately removed, and that there is no latent heat of freezing
However, lightning is caused by frozen condensates in an updraft!
We decided to test CAPE both ways—the traditional way, and with condensates/latent heat of freezing
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Image from NASA-GHCCWorldwide lightning climatology
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Traditional Lifted Index
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TEST Lifted Index
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Methodology
Goal: create a probabilistic lightning algorithm using a large set of CONUS observations and physical assumptions relevant worldwide 2006 3-hourly 20 km RUC analyses NLDN lightning in the RUC grid box (0-3 hr after
analysis) 3 hour precipitation from METARS
Find which forecast parameters are the best, then curve fit the probability of lightning given a binned value of that parameter
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2006 Results
METAR ObservationsNo lightning/no precip 2,014,877
No lightning/precip 147,881lightning/no precip 33,840
lightning/precip 27,143Total 2,223,741
Climatology of lightning 2.7%Climatology of lightning
given precipitation 15.5%Climatology of lightning given non-zero CAPE 4.1%
Climatology of lightning given precipitation and
non-zero CAPE 24.7%
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NLDN 3-hourly lightning climatology for a 16 km grid box (2003-2006)
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Results
GL CAPE is calculated from the LFC to -20C
Set to zero if equilibrium level is warmer than -20C
TEST is condensate and latent heat of freezing included
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CAPE > 0, Precipitation > 0.01
y = 0.14*Ln(x) + 0.005
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 50 100 150 200 250 300 350 400 450 500
CAPE (J/kg) * Precipitation (inches)Bins with width 5
Lig
htn
ing
Pro
bab
ilit
y
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CAPE=0, Precipitation > 0.01
y = 0.36x0.5
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
0 0.5 1 1.5 2 2.5 3 3.5 4
[LI in K (from -4 to 0) + 4] * Precipitation (inches)Bins width 0.10
Lig
htn
ing
Pro
ba
bili
ty
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CAPE > 0, Precipitation=0
y = 0.025Ln(x) + 0.03
0
0.02
0.04
0.06
0.08
0.1
0.12
0.14
0.16
0.18
0.2
0 5 10 15 20 25 30 35 40
CAPE / (CIN +100)
Lig
htn
ing
Pro
ba
bili
ty
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Results
Forecasts by bin when precipitation occurred
0
10000
20000
30000
40000
50000
60000
70000
80000
90000
0.025 0.075 0.125 0.175 0.225 0.275 0.325 0.375 0.425 0.475 0.525 0.575 0.625 0.675 0.725 0.775 0.825 0.875 0.925 0.975
Climatology=0.155
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Results
Reliability--Precipitation only
0
0.1
0.2
0.3
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0.5
0.6
0.7
0.8
0.9
1
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Forecast
Ob
se
rva
tio
ns Perfect Reliability
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Results
ROC Curve--precipitation only (probability thresholds on curve)
00.05
0.15
0.25
0.35
0.45
0.55
0.65
0.75
0.850.9510
0.1
0.2
0.3
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0.5
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0.7
0.8
0.9
1
0 0.2 0.4 0.6 0.8 1
FAR
PO
D
No Skill Forecast
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Method BSS ROC areaSPC -0.420 0.713NULL -0.180 0.500TEST 0.362 0.888
SPC method: forecast 100% chance of lightning if GL CAPE is greater than 100 J/kg and precipitation is greater than 0.01
inches. Forecast 0% otherwise.
NULL method: Always forecast 0% chance of lightning.
TEST method: Algorithm presented here.
BSS: Brier skill score, compares mean squared error of forecast to mean squared error of climatology. 1 is perfect, 0 is no skill,
negative is worse than climatology.
ROC area: Total integrated area underneath ROC curve. 1 is perfect, 0.5 is no skill.
Results
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Summary
Algorithm has been developed to forecast lightning probability given observed instability (RUC analysis) and precipitation (METARS)
Algorithm is somewhat sharp, reliable at all forecast probabilities, and has good resolution of events and non-events
Buoyancy calculations probably need to account for condensate and latent heat of freezing—but our data are not conclusive on this point
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Other/Future Work
Equations have been developed (not shown here) to forecast strikes per unit area for application to any model resolution
After knowing strikes per unit area, can forecast probabilities for smaller areas (i.e. Air Force base warning criteria area) based on downscaling climatology—equation has been developed for this purpose as well
Just beginning to look at algorithm with model data and in ensembles—issues with model precipitation forecasts
Acknowledgments: ARM data archive, Dr. Tony Eckel, Stephen Augustyn, Bill Roeder, Dr. David Bright, Jeff Cunningham
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Questions?
GFS 66 hour grid point lightning probability forecast valid this afternoon
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Backup Slides
Strikes per 400 square km
y = e4.5x
0
10
20
30
40
50
60
70
80
90
100
0 0.2 0.4 0.6 0.8 1
Probability
Str
ikes
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Backup Slides
Adjustments for changes in model resolution or area of interest First, re-calculate total number of strikes for the new
model grid box area If model grid is finer than RUC, re-calculate probabilities
using inverse of strikes equation If model grid is coarser than RUC, increase probabilities
using special upscaling equation If area of interest is smaller than area of model grid,
recalculate strikes and use downscaling equation to get probabilities
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Backup Slides
Downscaling equation details Inputs:
Strikes (S) horizontal resolution of coarse area in km (C) horizontal resolution of fine area in km (F)
Equation: 1-[1-(F^2/C^2)]^(S^A) Where A is a “fudge factor” depending on F A=1-0.17*LN(F-1)
A equals unity when F is 2 km, and slowly decreases toward zero as F approaches ~350 km
In nature, lightning tends to be randomly distributed at 2 km (storm scale) but more clustered at higher resolutions. “A” attempts to account for this
Best to use this equation from 2 to 128 km grid sizes If strikes is less than one, calculate equation using 1 strike, then multiply
result times number of strikes
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Backup Slides
Upscaling Probability added to:
[1-probability]*[1-(F^2/C^2)]*downscaled probability
This ensures high probabilities will only occur when the original probability was high, or the area has increased substantially with moderately high initial probabilities
No testing as to whether this is calibrated
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Backup SlidesNWS Topeka forecast taken from the web on 15 Aug:
Friday, August 17 at 7pmTemperature: 89°FThunder: <10%
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Backup Slides
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Backup Slides