Kevin Birk Mike Bardou and Mark Ratzer WFO Chicago Review of Two Storm Force Wind Events across Lake MI October 26 th Bomb December 12 th Winter Storm Both events produced Storm force winds 48 knots ID: 618442
Download Presentation The PPT/PDF document "Storm Force wind events of October and D..." is the property of its rightful owner. Permission is granted to download and print the materials on this web site for personal, non-commercial use only, and to display it on your personal computer provided you do not modify the materials and that you retain all copyright notices contained in the materials. By downloading content from our website, you accept the terms of this agreement.
Slide1
Storm Force wind events of October and December 2010
Kevin Birk, Mike Bardou and Mark RatzerWFO ChicagoSlide2
Review of Two Storm Force Wind Events across Lake MI
October 26th “Bomb”December 12th Winter StormBoth events produced Storm force winds (48+ knots).
However, the strength and the tracks of the two lows were quite different.Slide3
MotivationIncrease the forecast accuracy for the onset of high impact winds across Lake Michigan.
-> Gain a better understanding of the main processes that govern the onset and maintenance of storm force winds across the lake .Slide4
Central pressure dropped from 980 mb at 00UTC on the 26
th to 955 mb at 00UTC on the 27th as the surface low tracked across MN.
Lake MI remained in the warm sector through the morning of the 26th .
Occluded front pushed across the lake late morning on the 26
th
.
Following this, the system filled as the low became vertically stacked.
The October 26
th
BombSlide5
12 UTC Oct 26
th
00 UTC Oct 27
th
300 MB Jet and Surface
300 MB Jet and Surface Slide6
12 UTC Oct 27
th 00 UTC Oct 28th
300 MB Jet and Surface
300 MB Jet and Surface Slide7
12 UTC October 26th Slide8
15 UTC October 26
th Slide9
18 UTC October 26
th Slide10
21 UTC October 26
th Slide11
00 UTC October 27
th
Adiabatic Lapse RateSlide12
Forecasts For Oct 26th Event
Headlines for Gale/Storm watch first issued at 3:42 AM Sun 10/24Gale watch from Monday PM – Tuesday AM.Storm watch from Tuesday PM – Wed evening.Headlines upgraded to Storm Warning at 4:01 AM Mon 10/25. Warning from 4 AM Tue -7 PM Wed. Later forecasts shifted times slightly. Slide13
North Half Verification
Winds remained below Gale force Until about 10 AM Tue 26th as the cold front passed.Gusts remained below Storm force at the north buoy (peaked at 47 knots Tue PM). Port Inland, MI peaked at 56 knots Wed AM.
Frontal Passage
Frontal PassageSlide14
South Half Verification
Winds remained below Gale force Until about 7 AM Tue 26th as the cold front passed.Gusts remained below Storm force at the south buoy (peaked at 45 knots Tue PM). Chicago Harrison Crib peaked at 65 knots Tues AM.
Frontal PassageSlide15
December 12th Winter Storm
Surface Low tracked across Northern IL/Southern Lake MI during predawn hours on the 12th .The low deepened to 988 mb during the afternoon on the 12th as the low moved across western New York. Farther Northwest, Canadian high pressure of 1038 mb moved across eastern Dakotas.Slide16
12 UTC Dec 12
th
300 MB Jet and Surface
300 MB Jet and Surface
00 UTC Dec 13
th
Slide17
12 UTC December 12
th Slide18
15 UTC December 12
th Slide19
21 UTC December 12
th Slide20
03 UTC December 13
th Slide21
03 UTC December 13
th
Super Adiabatic Lapse RateSlide22
Forecasts For Dec 12th Event
Headlines for Gale/Storm watch first issued at 8:50 AM December 10th. Late Saturday the 11th through Monday morning the 13th. Winds to 55 knots on Sunday/Sunday Night the 12th .
Headlines upgraded to Storm Warning at 2:27 PM on the 11th .
Late Saturday the 11
th
through Monday morning the 13
th
.
Winds to 55 knots on Sunday/Sunday Night the 12th .Slide23
Verification
North Half
Winds increased to Gales around 04 UTC and to Storm by 10 UTC.
Storm force winds ended around 11 UTC on the 13
th
(25 hours of storm).
South Half
Winds increased to Gales/Storm around 14 UTC.
Storm force winds ended around 05 UTC on the 13
th
(15 hours of storm).Slide24
ConsiderationsStability over the lake
Boundary layer lapse rates.Near adiabatic -> gusts = boundary layer winds.Super adiabatic -> gusts = the max wind in the boundary layer.The track of the low and time of year. Strength of cold air advection.Dynamics Isallobaric wind component.
Synoptic scale descent following the passage of a mid level vorticity max and dry slot. Slide25
Questions?