TDS look-alike signatures along the leading edge of QLCSs and implications for warning decisions
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1 TDS look-alike signatures along the leading edge of QLCSs and implications for warning decisions 3 rd Midwest Bow Echo Workshop March 2017 St. Louis, MO Lewis Kanofsky NWS St. Louis, MO
2 1817z
3 1817z
4 1817z
5 1817z WarnGen
6 Issue a tornado warning? YES NO
7 Issue a tornado warning? Radar Environment Spotters (no reports) YES NO
8 Issue a tornado warning? Radar Environment Spotters (no reports) YES Radar Environment Spotters (no reports) NO
9 #SafePlaceSelfie
10 Issue a tornado warning? Need an extra piece of information to tip the scales YES NO
11 1825z Z V ZDR CC
12 1825z Z V ZDR CC
13
14 Tornadic Debris Signature (TDS) Required CC reduction* Appropriate velocity signature High enough Z** Admired (but not required) Spatial and temporal continuity May or may not be present ZDR near zero * CC 0.70 or 0.80 in some studies ** Z threshold varies by study, typically dbz
15 * CC 0.70 or 0.80 in some studies ** Z threshold varies by study, typically dbz *** ZDR 0.5 in some studies Tornadic Debris Signature (TDS) Required CC reduction* Appropriate velocity signature High enough Z** Admired (but not required) Spatial and temporal continuity May or may not be present ZDR near zero***
16 1825z Z V dbz Mesovortex ZDR CC
17 Other processes can mimic a TDS
18 Other processes can mimic a TDS Required CC reduction Appropriate velocity signature High enough Z (sometimes) Admired (but not required) Spatial and temporal continuity (sometimes) May or may not be present ZDR near zero
19 Other processes can mimic a TDS 8 Apr 2015
20 Other processes can mimic a TDS 8 Apr 2015
21 Other processes can mimic a TDS Inflow 8 Apr 2015 Inflow
22 Other processes can mimic a TDS 8 Apr 2015
23 Other processes can mimic a TDS Non-uniform beam filling (NBF) 8 Apr 2015
24 Other processes can mimic a TDS
25 Other processes can mimic a TDS 17 Nov 2013
26 Other processes can mimic a TDS 17 Nov 2013
27 Other processes can mimic a TDS 17 Nov 2013
28 Other processes can mimic a TDS Low SNR 17 Nov 2013
29 Other processes can mimic a TDS Low SNR Non-uniform beam filling (NBF) 17 Nov 2013
30 Not a TDS 1. Inflow region of a supercell 2. Non-uniform beam filling 3. Hail spikes downstream 4. Side lobe contamination (vertical or horizontal)
31 TDS Not a TDS Increased confidence in a tornado
32 TDS Not a TDS Increased confidence in a tornado WFO actions
33 TDS Not a TDS Increased confidence in a tornado WFO actions Partner actions
34 TDS Not a TDS Increased confidence in a tornado WFO actions Partner actions Public response
35 TDS Not a TDS Increased confidence in a tornado WFO actions Partner actions Public response
36 1825z Z V ZDR CC This static image alone isn t enough
37 Watching multiple mesos? Easy to be startled when a new slice comes in (especially with MESO-SAILS)
38 Watching multiple mesos? Easy to be startled when a new slice comes in (especially with MESO-SAILS) Key question: how did the imagery evolve?
39 Why it s not a TDS
40 Notch, nub, or hook Pre-existing ribbon of low CC along the leading edge
41
42
43 Ribbon of low CC wraps back into the meso
44 Area of low CC becomes closed off
45 Not a TDS
46 Not a TDS CC isn t low because of debris.
47 26 Apr z 0.5 Z V ZDR CC
48 26 Apr z 0.5 Z V ZDR CC
49 26 Apr z 0.5 Z V ZDR CC
50 26 Apr z 0.5 Z V ZDR CC
51 26 Apr z 0.5 Z V ZDR CC
52 26 Apr z 0.5 Z V ZDR CC
53 26 Apr z 0.5 Z V ZDR CC
54 Damage survey results Extensive damage survey Widespread 80 mph wind damage 2 weak tornadoes No tornadoes associated with this CC feature
55 Comparison with a real TDS
56 Notch, nub, or hook CC may be noisy along the leading edge, but it s not a clear ribbon
57
58 Area of low CC appears suddenly
59
60 TDS CC is low because of debris.
61 01 Jun z 0.5 Z V ZDR CC
62 01 Jun z 0.5 Z V ZDR CC
63 01 Jun z 0.5 Z V ZDR CC
64 01 Jun z 0.5 Z V ZDR CC
65 01 Jun z 0.5 Z V ZDR CC
66 01 Jun z 0.5 Z V ZDR CC
67 01 Jun z 0.5 Z V ZDR CC
68 01 Jun z 0.5 Z V ZDR CC
69 Damage survey results EF-3 Track passed within 1 mile of WFO St. Louis
70 Implications for warning decisions Spot a potential TDS? Take a few seconds to step back and forth. Ask: how did the radar imagery get to this point?
71 Unresolved questions
72 Unresolved questions Physically, what causes the ribbon of low CC?
73 Unresolved questions Physically, what causes the ribbon of low CC? Why some QLCSs but not others?
74 Unresolved questions Physically, what causes the ribbon of low CC? Why some QLCSs but not others? Why doesn t the return signal from the rain dominate the pulse volume after the ribbon of low CC has wrapped back into the meso?
75 Unresolved questions Physically, what causes the ribbon of low CC? Why some QLCSs but not others? Why doesn t the return signal from the rain dominate the pulse volume after the ribbon of low CC has wrapped back into the meso? Why does this zone retain an independent identity? (Why doesn t it mix?)
76 Unresolved questions Is this feature unique to QLCSs or does it also occur with supercells?
77 Unresolved questions Is this feature unique to QLCSs or does it also occur with supercells? If a tornado occurs in the closed-off area and lofts debris, would CC decrease further, or is it a blind spot for radar operators (unable to detect tornadoes because CC is already low)?
78 Take-home messages TDS Not a TDS Increased confidence in a tornado WFO actions Spot a potential TDS? Ask: how did the radar imagery evolve? Partner actions Public response
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