warm-season lake-/sea-breeze severe weather in the northeast patrick h. wilson, lance f. bosart, and...

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Warm-Season Lake-/Sea- Breeze Severe Weather in the Northeast Patrick H. Wilson, Lance F. Bosart, and Daniel Keyser Department of Earth and Atmospheric Sciences, University at Albany, Albany, NY Thomas A. Wasula NOAA / National Weather Service, Albany, NY CSTAR II Grant NA04NWS4680005 Northeast Regional Operational Workshop VIII Presentation 2 November 2006

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Warm-SeasonLake-/Sea-Breeze Severe Weatherin the Northeast

Patrick H. Wilson, Lance F. Bosart, and Daniel KeyserDepartment of Earth and Atmospheric Sciences, University at Albany, Albany, NY

Thomas A. WasulaNOAA / National Weather Service, Albany, NY

CSTAR II Grant NA04NWS4680005

Northeast Regional Operational Workshop VIII Presentation

2 November 2006

Research Goals

Investigate thermodynamical and dynamical processes along with physiographic effects

Increase understanding of this phenomenon

Methodology – Part I

Warm-Season: April – October

Domain: OH, PA, MD, DE, NJ, NY, VT, NH, MA, CT, RI, ME

Selected cases from Storm Prediction Center archived storm data 2000-present

Verified from National Climatic Diagnostic Center archived radar data

Methodology – Part II

Obtained NCEP/NARR gridded datasets for each case and plot important weather variables

Collected soundings, radar data, and surface observations

Classified cases into separate categories and conducted case study analyses

Case Classifications

Pure Case: mesoscale forcing primary;

synoptic-scale forcing secondary

Mixed Case: mesoscale forcing and synoptic-

scale forcing working together

Null Case: convection suppressed by

lake-/sea-breeze processes

Case List

Pure Cases

9 August 2001 (Ontario)

6 July 2003 (Erie)

7 August 2005 (Chesapeake)

2 August 2006 (Ontario)

Mixed Cases

9 April 2001 (Erie)

19 June 2002 (Atlantic)

24 July 2003 (Erie and Ontario)

1 August 2005 (Huron and Ontario)

24 April 2006 (Chesapeake)

Null Case11 July 2006 (Atlantic)

1200 UTC 9 August 2001 (Pure Case)

30 35 40 45 50 55 60 65 70

1200 UTC 9 August 2001

14 18 22 26 30 34 38 42 46

1200 UTC 9 August 2001

1200 UTC 9 August 2001http://weather.uwyo.edu/upperair/sounding.html

Note:

Parcel taken from lowest 500 m to determine CAPE

1500 UTC 9 August 2001

-14 -12 -10 -8 -6 -4 -2 0

1800 UTC 9 August 2001

340 345 350 355 360 365 370 375 380

1800 UTC 9 August 2001

-3.5 -3.0 -2.5 -2.0 -1.5 -1.0 -0.5 0.0

1700 UTC 9 August 2001

1700 UTC 9 August 2001 Radar Composite

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1800 UTC 9 August 2001 Radar Composite

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1900 UTC 9 August 2001 Radar Composite

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2000 UTC 9 August 2001 Radar Composite

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2100 UTC 9 August 2001 Radar Composite

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2200 UTC 9 August 2001 Radar Composite

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2300 UTC 9 August 2001 Radar Composite

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0000 UTC 10 August 2001 Radar Composite

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0100 UTC 10 August 2001 Radar Composite

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0200 UTC 10 August 2001 Radar Composite

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9 August 2001 Storm Reports

Pure Cases:Preliminary Conclusions

Ridge axis in place at the surface or aloft

Low unidirectional wind shear in low-levels (< 10 m s-1 for 925-700 hPa layer)

T > 30°C, Td > 20°C, CAPE > 1500 J kg-1

Placement and timing signal by θe-ridge axis (θe > 335 K)

Intersections of boundaries enhance convection

Tendency to become squall lines and prefer valleys

Occur most often during hottest months of summer

1200 UTC 19 June 2002 (Mixed Case)

30 35 40 45 50 55 60 65 70

1200 UTC 19 June 2002

14 18 22 26 30 34 38 42 46

1200 UTC 19 June 2002

1200 UTC 19 June 2002http://weather.uwyo.edu/upperair/sounding.html

Note:

Parcel taken from lowest 500 m to determine CAPE

1500 UTC 19 June 2002

-14 -12 -10 -8 -6 -4 -2 0

1800 UTC 19 June 2002

320 325 330 335 340 345 350 355 360

1800 UTC 19 June 2002

1800 UTC 19 June 2002 Radar Composite

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1900 UTC 19 June 2002 Radar Composite

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2000 UTC 19 June 2002 Radar Composite

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19 June 2002 Storm Reports

Mixed Cases:Preliminary Conclusions

Troughs generally in place at the surface or aloft

Typically more wind shear (speed shear and veering winds) in low levels

20°C < T < 30°C, 10°C < Td < 20°C, θe > 320 K

Cyclonic vorticity and cyclonic vorticity advection important

Intersection of boundaries enhance convection

Occur most often during late spring and early autumn

1800 UTC 11 July 2006 (Null Case)

330 335 340 345 350 355 360 365 370

1800 UTC 11 July 2006

1800 UTC 11 July 2006 Radar Composite

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11 July 2006 Storm Reports

Lake and sea breezes can suppress convection.

1800 UTC 6 July 2003 MODIS Satellitehttp://rapidfire.sci.gsfc.nasa.gov/realtime/

Questions?