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Water Level Monitoring and Flood Hazard Emergency Management in Chesapeake Bay John D. Boon John M. Brubaker Virginia Institute of Marine Science C.R. Berquist Department of Geology, College of William and Mary

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  • Water Level Monitoring and Flood Hazard Emergency

    Management in Chesapeake BayJohn D. Boon John M. Brubaker

    Virginia Institute of Marine Science

    C.R. BerquistDepartment of Geology, College of William and Mary

  • Should we care about climate

    change?

  • Jamestown Water Levels and Flood Hazard Emergency Management Project

    Project Goals:• To provide emergency managers with water

    level data in near real-time during tropical storm and hurricane events via the Internet

    • Establish a data base of measured water level extremes as an aid to community planning

    • Provide water level histories needed to verify numerical models

  • 7 OCT 2006 ‘NORTHEASTER’ www.worldtidesandcurrents.com

    Photo courtesy of Dr. David Forrest, VIMS

    www.vims.edu/physical/

  • Jamestown Water Levels and Flood Hazard Emergency Management Project

    Project Goals:• To provide emergency managers with water level data

    in near real-time during tropical storm and hurricane events via the Internet

    • Establish a data base of measured water level extremes as an aid to community planning

    • Provide water level histories needed to verify numerical models

  • Jamestown Water Levels and Flood Hazard Emergency Management Project

    Project Goals:• To provide emergency managers with water level data

    in near real-time during tropical storm and hurricane events via the Internet

    • Establish a data base of measured water level extremes as an aid to community planning

    • Provide water level histories needed to verify numerical models

  • In the coastal zone, extreme flooding is caused by

    STORM TIDES

  • Storm Tide:Sum of a Storm Surge and the

    Astronomical Tide

    Storm Surge: Water level change due to storm effects (wind, low pressure)

    Astronomical Tide: Water rise and fall due to gravity of earth, moon and sun

  • ERNESTO Storm Surge: 3.56 feet

  • Storm Tide: 5.51 feet

  • What a Difference a “Phase” Makes …

    September, 2006

  • 8/318/318/318/31 9/19/19/19/1 9/29/29/29/2 9/39/39/39/30000

    1111

    2222

    3333

    4444

    5555

    6666Hampton Roads (Sewells Pt), VA

    storm tideastronomical tidestorm surgemmsl (lunar)

    2006

    ‘ERNESTO’

  • 8/318/318/318/31 9/19/19/19/1 9/29/29/29/2 9/39/39/39/30000

    1111

    2222

    3333

    4444

    5555

    6666

    Windmill Point, VA

    storm tideastronomical tidestorm surgemmsl (lunar)

    Water Level (feet above MLLW)

    2006

    ‘ERNESTO’

  • 50 Years of Storm Tides at Sewells Point

    1957 – 2006Four Northeasters and a Hurricane

  • Water levels from U.S. National Oceanic and Atmospheric Administration

  • Sea Level Change at Hampton Roads, Virginia

    1930 - 2005

  • -0.5

    0.0

    0.5

    1.0

    1.5

    2.0

    2.5

    3.0

    1930

    1934

    1939

    1943

    1948

    1952

    1956

    1961

    1965

    1970

    1974

    1979

    1983

    1987

    1992

    1996

    2001

    Fee

    t ab

    ove

    198

    3-20

    01 M

    LL

    W Monthly Mean Sea Level, Hampton Roads (Sewells PT), VA

    Sea Level Trend: 1.4 ft/century

  • -0.5

    0.0

    0.5

    1.0

    1.5

    2.0

    2.5

    3.0

    1930

    1934

    1939

    1943

    1948

    1952

    1956

    1961

    1965

    1970

    1974

    1979

    1983

    1987

    1992

    1996

    2001

    Fee

    t ab

    ove

    198

    3-20

    01 M

    LL

    W Monthly Mean Sea Level, Hampton Roads (Sewells PT), VA

    Sea Level Trend: 1.4 ft/century

    Aug33

    Sep03

    Sep44Oct54Aug55

    Sep60Mar62

    Sep99

    Water levels from U.S. National Oceanic and Atmospheric Administration

  • Lower Chesapeake Bay Storm Tide Comparisons‘ERNESTO’ - September, 2006

    Northeaster – October, 2006Northeaster – November, 2006

  • Extratidal High Water (XHW)

    A new metric for comparing storm tides

  • HAT

    LAT

  • HAT

    LAT

    ? ? ?

  • HAT

    LAT

    0.83

  • 1.98 feet

    HAT

    EXTRATIDAL HIGH WATER

    LAT

    0.83

  • JAMES RIVER (SEWELLS POINT)

    0

    1

    2

    3

    4

    5

    6

    Sep-06 Oct-06 Nov-06

    EX

    TRA

    TID

    AL

    HIG

    H W

    ATE

    R Feet

    ‘ERNESTO’

  • RAPPAHANNOCK RIVER (WINDMILL POINT)

    0

    1

    2

    3

    4

    5

    6

    Sep-06 Oct-06 Nov-06

    EX

    TRA

    TID

    AL

    HIG

    H W

    ATE

    RFeet

    ‘ERNESTO’

  • YORK RIVER (USCG TRAINING CENTER)

    0

    1

    2

    3

    4

    5

    6

    Sep-06 Oct-06 Nov-06

    EX

    TRA

    TID

    AL

    HIG

    H W

    ATE

    R

    Feet

    ‘ERNESTO’

  • November 2006

  • YORK RIVER (USCG TRAINING CENTER)

    0

    1

    2

    3

    4

    5

    6

    Sep-06 Oct-06 Nov-06

    EX

    TRA

    TID

    AL

    HIG

    H W

    ATE

    R

    Feet

    ‘ERNESTO’

    2.5

  • HURRICANES

    0

    1

    2

    3

    4

    5

    6

    AUG, 1933 ISABEL KATRINA

    EX

    TRA

    TID

    AL

    HIG

    H W

    ATE

    R

    Feet

  • Work in Progress at Jamestown …

    Jamestown water level station