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2009 Storms, Part 2
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2009 Storms, Part 2
1.
2009 StormsPart 2
©2010 Fisher
2.
3.
Radar beam increases
in size with distance from radar.
4.
Radar takes 4-5
minutes to complete full scan when in storm/precip mode.
5.
Reliable doppler wind
data limited to about 60-70 nm.
6.
7.
Height of beam
above ground vs distance from radar. Green 10nm Yellow 15nm Red 20nm
8.
MDW TDWR 20nm
10nm
9.
ORD TDWR 20nm
10nm
10.
11.
PROBLEM(s) OF THE
DAY (POTD) ORGANIZED SEVERE STORMS INGREDIENTS-BASED APPROACH MOISTURE INSTABILITY (sources for convective) LIFT SHEAR
12.
13.
TornadicSupercell “Ingredients” Instability
(varies, usually CAPE > 1000 J/Kg) Deep layer shear (0-6km) bulk shear > 35kt Low level shear (0-1km) SRH > 150 m2/s2 or pre-existing boundary) Relatively high RH values (in BL and aloft) Sfc Td depressions <12°F
14.
15.
Effective Bulk Shear
(EBS)
16.
Supercell Composite Parameter
(SCP)
17.
18.
Showed boldly only
after event started
19.
Underscores STP as
a DIAGNOSTICparameter
20.
0-6 km shear,
0-1 km SRH (400+), and MLLCL all favorable for STP ≥1
21.
Primary shortcoming resulted
from MLCAPE values less than 500 J/kg until 23z
22.
23.
24.
25.
26.
27.
28.
29.
30.
31.
32.
33.
34.
35.
Friday June 19,
2009 Naper Days
36.
37.
38.
39.
Pocket of 87
mph winds
40.
41.
42.
43.
44.
45.
46.
July 24, 2009
47.
48.
49.
50.
ILX
51.
ILX
52.
Base Velocity 1700
ft
53.
3500 ft
54.
LOT
55.
56.
Base Velocity
57.
58.
Aug. 9, 2009
59.
DVN
60.
61.
DVN Base Velocity
62.
DVN Storm Relative
Velocity
63.
DVN VAD Wind
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