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Flash Flood Events associated with Northeastern Cutoff Cyclones. Derek V. Mallia and Nicholas D. Metz University at Albany Department of Atmospheric and Environmental Sciences 35 th Northeast Storms Conference, Saratoga Springs, NY 7 March 2010. Outline:. Methodology

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Flash flood events associated with northeastern cutoff cyclones

Flash Flood Events associated with Northeastern Cutoff Cyclones

Derek V. Mallia and Nicholas D. Metz

University at Albany

Department of Atmospheric and Environmental Sciences

35th Northeast Storms Conference, Saratoga Springs, NY

7 March 2010


Outline
Outline: Cyclones

  • Methodology

  • Climatology of flash flood (FF) producing cutoff cyclones

    • monthly distribution

    • mean location relative to moisture transport

    • forcing mechanisms

  • Case Study

    • 250-hPa wind analysis

    • 500-hPa height and vorticity analysis

    • 850-hPa wind and precipitable water analysis

  • Conclusion


  • Data sources
    Data Sources Cyclones

    • Earth System Research Laboratory (ESRL) daily composites

    • Rapid Update Cycle (RUC20)

    • Advanced Weather Information Processing System (AWIPS)

    • Weather Event Simulator (WES)

    • Geostationary Operational Environmental Satellite (GOES)

    • Albany Radar (KENX)


    Methodology
    Methodology Cyclones

    • Examined warm season FF events that were associated with convection (May through September)

    • FF event defined as one or more days under a similar weather feature with at least one FF report verified by the National Weather Service

    • A widespread FF event is defined as multiple FF reports that are separated by at least 40 km

    • An isolated FF event is defined as a one or more FF reports that occur within 40 km


    Methodology cont
    Methodology (cont.) Cyclones

    • Only events with a closed height contour at the 850 & 300 hPa levels were considered for the FF cutoff cyclone climatology

    • Cutoff cyclones had a minimum depth of 30 meters at 850 hPa and were cutoff for at least 24 hours


    Methodology cont1
    Methodology (cont.) Cyclones

    • Dataset consists of FF and cutoff cyclone events that affected the Albany County Warning Area (CWA) between the years 2003 and 2009 that meet previous criteria listed


    Ff producing cutoff cyclone climatology
    FF-Producing Cutoff Cyclone Climatology Cyclones

    • Out of the 39 FF days in the Albany CWA between 2003-2009, 11 were the result of cutoff cyclones

    • Out of these 11 FF days that resulted from a cutoff cyclone, 8 were considered widespread incidents while 3 remained isolated

    • Out of the 7 cutoff FF events, 3 resulted in multiple days of FF reports


    Frequency of cutoffs and ff producing cutoffs that affect the albany cwa 2003 2009
    Frequency of Cutoffs and FF Producing Cutoffs that affect the Albany CWA (2003-2009)

    - Cutoffs

    - FF Producing Cutoffs

    Number of Cutoffs

    Months


    Precipitable Water the Albany CWA Normals and Departures for Albany, NY

    Precipitable Water (mm)

    Months


    Mean 500 hpa geopotential heights for ff producing cutoff cyclones
    Mean 500-hPa geopotential heights for FF producing cutoff cyclones

    Composite of flash flood producing cutoff cyclone events

    (m)

    N=11


    Cutoff Cyclone Tracks cyclones

    Tom Wasula et al, 2009


    Mean 250 hpa vector winds for ff producing cutoff cyclones
    Mean 250-hPa vector winds for FF producing cutoff cyclones cyclones

    Composite of flash flood producing cutoff cyclone events

    (m s1)

    N=11


    Mean 850 hpa meridional winds for ff producing cutoff cyclones
    Mean 850-hPa meridional winds for FF producing cutoff cyclones

    Composite of flash flood producing cutoff cyclone events

    (m s1)

    N=11


    Anomalous 850 hpa meridional winds for ff producing cutoff cyclones
    Anomalous 850-hPa meridional winds for FF producing cutoff cyclones

    Composite of flash flood producing cutoff cyclone events

    (m s1)

    N=11


    Precipitable water anomaly cyclonesfor FF producing cutoff cyclones

    Composite of flash flood producing cutoff cyclone events

    (kg m2)

    N=11


    Mean 700-hPa vertical motion for FF producing cutoff cyclones

    Composite of flash flood producing cutoff cyclone events

    (Pa s1)

    N=11


    Neutral Type A Tilt cyclones

    Tom Wasula et al, 2009



    Ff producing cutoff cyclones what to look for
    FF Producing Cutoff Cyclones: cyclonesWhat to Look for…

    • Great Lakes track cutoff cyclone with a Neutral Tilt Type A

    • Anomalously strong meridional flow coming off the Atlantic Ocean which provides a sufficient moisture transport for storms

    • Forcing mechanism from either an upstream vorticity maximum, surface boundary, or favorable position in local jet max

    • Low to moderate amounts of instability and CAPE sufficient enough to cause a flash flood event



    Synopsis of the 30 june 1 july 2009 ff event
    Synopsis of the 30 June–1 July 2009 FF Event cyclones

    • Widespread FF event

      • 13 reports total

  • Occurred in the following counties:

    • Albany

    • Columbia

    • Bennington

    • Montgomery

    • Rensselaer

    • Saratoga

    • Schenectady

    • Ulster

    • Washington

  • Multiple day event

  • Associated with cutoff cyclone over Lake Ontario


  • 30 june day 1
    30 June (Day 1) cyclones

    • Consisted of 3 FF reports in the following counties (3 reports)

      • Bennington (1 report)

      • Montgomery (1 report)

      • Ulster (1 report)

  • FF reports occurred between 1700–2300 UTC

  • Significant severe weather event as there were multiple large hail and wind reports throughout the CWA


  • CAPE: cyclones1,753 J/kg

    PWAT: 31.2 mm

    Dewpoint: 17 C

    K index: 32

    Freezing level: 3,293 m




    1200 utc 30 june 2009
    1200 UTC 30 June 2009 cyclones

    500 hPa Heights (dam), Absolute Vorticity (> 16  105 s1), and Wind barbs (kt)


    1800 utc 30 june 2009
    1800 UTC 30 June 2009 cyclones

    500 hPa Heights (dam), Absolute Vorticity (> 16  105 s1), and Wind barbs (kt)


    2100 utc 30 june 2009
    2100 UTC 30 June 2009 cyclones

    200 hPa Heights (dam),Wind Speed (kt), and Wind barbs (kt)


    1800 utc 30 june 20091
    1800 UTC 30 June 2009 cyclones

    Precipitable Water (mm), and 850-hPa Wind barbs (kt)


    2100 utc 30 june 20091
    2100 UTC 30 June 2009 cyclones

    Precipitable Water (mm), and 850-hPa Wind barbs (kt)


    1 july day 2
    1 July (Day 2) cyclones

    • Consisted of FF reports in the following counties (10 reports)

      • Albany (2 reports)

      • Columbia (1 report)

      • Rensselaer (1 report)

      • Saratoga (2 reports)

      • Schenectady ( 3 reports)

      • Washington (1 report)

  • FF reports occurred between 1900–2200 UTC

  • Significant flash flooding


  • CAPE: cyclones1,914 J/kg

    PWAT: 31.2 mm

    Dewpoint: 18 C

    K index: 32

    Freezing level: 3,192 m


    1500 utc 1 july 2009
    1500 UTC 1 July 2009 cyclones

    500 hPa Heights (dam), Absolute Vorticity (> 16  105 s1), and Wind barbs (kt)


    1800 utc 1 july 2009
    1800 UTC 1 July 2009 cyclones

    500 hPa Heights (dam), Absolute Vorticity (> 16  105 s1), and Wind barbs (kt)


    1500 utc 1 july 20091
    1500 UTC 1 July 2009 cyclones

    200 hPa Heights (dam),Wind Speed (kt), and Wind barbs (kt)


    1800 utc 1 july 20091
    1800 UTC 1 July 2009 cyclones

    200 hPa Heights (dam),Wind Speed (kt), and Wind barbs (kt)


    1500 utc 1 july 20092
    1500 UTC 1 July 2009 cyclones

    Precipitable Water (mm), and 850-hPa Wind barbs (kt)


    1800 utc 1 july 20092
    1800 UTC 1 July 2009 cyclones

    Precipitable Water (mm), and 850-hPa Wind barbs (kt)


    Conclusions
    Conclusions: cyclones

    • FF producing cutoff cyclones generally occur during June, July, & August and track across the Great Lakes

    • Cutoff cyclone FF events often result in multi-day, widespread incidents due to slow progression of the cyclones and/or antecedent weather conditions

    • FF producing cutoff cyclones tend to occur near anomalously strong moisture transport with forcing for ascent associated with upstream vorticity maxima and upper-level jet stream

    • Neutral tilt Type A most favorable type of cutoff cyclone for flash flooding


    Acknowledgements
    Acknowledgements cyclones

    • Joe Villani; NWS Albany

    • Tom Wasula; NWS Albany

    • Neil Stuart; NWS Albany

    • Ross Lazear; University at Albany

    • Alan Srock; University at Albany

    • Jonas Asuma; University at Albany

    • Kyle MacRichie; University at Albany

    • Kyle Griffin; University at Albany

    • And my classmates!



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