results from vaisala’s long range lightning detection network (lldn) tropical cyclone studies

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Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies Nicholas W. S. Demetriades Applications Manager, Meteorology Business Area Vaisala, Inc. Monterey, CA 24 March 2009

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Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies. Nicholas W. S. Demetriades Applications Manager, Meteorology Business Area Vaisala, Inc. Monterey, CA 24 March 2009. Hurricane Rita (2005). Demetriades and Holle (2008) Introduction - Goal. - PowerPoint PPT Presentation

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Page 1: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

Nicholas W. S. Demetriades

Applications Manager, Meteorology Business Area

Vaisala, Inc.

Monterey, CA

24 March 2009

Page 2: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 2

Hurricane Rita (2005)

Page 3: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 3

Demetriades and Holle (2008)Introduction - Goal

• Study inner core lightning rates throughout the full lifecycle of Atlantic tropical cyclones for a large sample size

Page 4: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 4

Methodology

• Full lifecycle of tropical cyclones that occurred in Atlantic basin from 2004 through 2007

• Landfall not excluded

• Subtropical storms not studied

• Tropical cyclone position and maximum sustained wind speeds obtained from National Hurricane Center best track data

• Interpolated positions and maximum sustained wind speeds between 6-hour intervals to obtain 3-hour values

• Tropical cyclone inner core lightning defined as 3-hourly CG lightning flash rates within 100 km of center of storm position

• Day/Night detection efficiency corrections were applied

Page 5: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 5

MethodologyTropical cyclone intensity categories

Tropical cyclone intensity category Maximum sustained wind speeds

Tropical depression (TD) <35 knots

Tropical storm – weak (TS-W) 35-49 knots

Tropical storm – strong (TS-S) 50-63 knots

Hurricane – weak (H-W) 64-95 knots

Hurricane – strong (H-S) >95 knots

Page 6: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 6

Atlantic basin resultsDay/Night, DE-corrected cumulative lightning rate distribution table

Tropical cyclone intensity category

Sample size Percentile of first non-zero

lightning count

50th percentile 75th percentile 90th percentile

Tropical depression (TD)

480 42% 3 100 585

Tropical storm – weak (TS-W)

658 35% 18 280 1248

Tropical storm – strong (TS-S)

446 29% 24 477 1765

Hurricane – weak (H-W)

512 47% 2 43 276

Hurricane – strong (H-S)

373 29% 16 76 200

Page 7: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 7

Atlantic basin resultsInner core lightning with respect to landfall

0

50

100

150

200

250

300

350

400

-24 -21 -18 -15 -12 -9 -6 -3 0 3 6 9 12 15 18 21 24

Time in hours with respect to landfall (time zero)

3-h

ou

r in

ne

r c

ore

lig

htn

ing

ra

te

Median 75th percentile

Page 8: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 8

Conclusions

• New finding: Atlantic tropical cyclones produce the highest inner core lightning rates during the tropical storm stage and the lowest inner core lightning rates during the hurricane stage

• High inner core (eyewall) lightning rates occur infrequently in category 3-5 hurricanes

• Appear to be related to eyewall replacement cycles (Knabb et al., 2008)

• Atlantic tropical cyclones produce more inner core lightning during the 24-hour period leading up to, and including landfall, than they do during the 24-hour period after landfall

Page 9: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 9

Hurricane Katrina (2005)Eyewall replacement & Continuous eyewall lightning

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Date and Time (M/D/YYYY HHmm) UTC

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ou

r e

ye

wa

ll lig

htn

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ra

te

0

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Ma

xim

um

su

sta

ine

d w

ind

sp

ee

d (

kn

ots

)

Uncorrected Day/Night DE Corrected Maximum Sustained Wind Speed

Page 10: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 10

Hurricane Wilma (2005)Eyewall replacement

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ou

r e

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wa

ll lig

htn

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ra

te

0

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80

100

120

140

160

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Ma

xim

um

su

sta

ine

d w

ind

sp

ee

d (

kn

ots

)

Uncorrected Day/Night DE Corrected Maximum Sustained Wind Speed

Page 11: Results from Vaisala’s long range lightning detection network (LLDN) tropical cyclone studies

©Vaisala | date | Ref. code | Page 11

Hurricane Felix (2007)Eyewall replacement

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Date and Time (M/D/YYYY HHmm) UTC

3-h

ou

r e

ye

wa

ll lig

htn

ing

ra

te

0

20

40

60

80

100

120

140

160

Ma

xim

um

su

sta

ine

d w

ind

sp

ee

d (

kn

ots

)

Uncorrected Day/Night DE Corrected Maximum Sustained Wind Speed