Stormtrack WRF - Oklahoma and Texas
10 km / 31 hybrid sigma layers / 200 mb ceiling / Grell-Devenyl cumulus / WSM6 precipitation
H250 Mass divergence
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H250 Height/RH%
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H250 Height/temperature
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H250 Q-vector
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H250 Wind
00
01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H500 Height/RH%
00
01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H500 Height/vorticity
00
01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H500 Height/temperature
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H500 Omega diagnostic
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H500 Height/vorticity
00
01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H700 Height/RH%
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H700 Height/temperature
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H850 Height/RH%
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
H850 Height/temp
00
01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
SFC convergence
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
SFC dewpoint
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
SFC temperature
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
SFC wind
00
01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
CAPE (Convective Energy)
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
CIN (Convective Inhibition)
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
Mean layer RH%
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
Precipitation
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01
02
03
04
05
06
07
08
09
10
11
12
13
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16
17
18 HR
Radar reflectivity
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
SREH (Storm relative helicity)
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
Storm motion (Bunkers method)
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01
02
03
04
05
06
07
08
09
10
11
12
13
14
15
16
17
18 HR
