Introduction to Storm Surge

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Transcription:

Introduction to Storm Surge

Hurricane Katrina (2005) Mississippi 1200 deaths, $108 billion damage

Hurricane Sandy (2012) Northeast U.S. 73 deaths, $65 billion damage

Hurricane Ike (2008) - Bolivar Peninsula, Texas 20 deaths, $29.5 billion

Unit Outline Introduction to Storm Surge Who is vulnerable? What is Storm Surge? Factors affecting Storm Surge Measuring Storm Surge

Ike s track

House of David and Kimberly King Waveland, Mississippi

Vulnerability Coastal areas are at increasing risk from sea-level rise and storm surge Rising sea-level provides a higher base for future surge/inundation events thus producing an increasing threat to: Coastal communities Ecosystems (wetlands, critical species, habitat loss, etc) Transportation systems (highway systems, ports, rail) Economic viability (tourism, transport of goods, natural resources) Energy

Gulf Coast Biloxi, Mississippi Katrina (2005) Key West, Florida Georges (1998) Laffite, Louisiana Rita (2005) Galveston, Texas Ike (2008)

Southeast Rodanthe, North Carolina Isabel (2003) Pawley s Island, South Carolina Hugo (1989) Jacksonville, Florida Fay (2008) North Hutchinson Island, Florida (Jeanne 2004)

Mid-Atlantic Baltimore, Maryland Isabel (2003) Hampton, Virginia Isabel (2003) Mantoloking, New Jersey Sandy (2012) Staten Island, New York (Sandy 2012)

New England Narragansett Bay, Rhode Island Carol (1954) Westport, Massachusetts Irene (2011) Providence, Rhode Island 1938 Hurricane East Haven, Connecticut Sandy (2012)

What is Storm Surge? STORM SURGE is an abnormal rise of water generated by a storm, over and above the predicted astronomical tide. STORM TIDE is the water level rise during a storm due to the combination of storm surge and the astronomical tide

Storm Surge from Hurricane Irene Rumley Marsh on the Pamlico River in North Carolina

Low Water from Hurricane Irene Pamlico Sound at Cape Hatteras, NC

Storm Surge from Tropical Storm Debby Bayshore Blvd., Tampa, FL

Storm Surge from Hurricane Isaac Pontchartrain Drive, Slidell, LA

Typhoon Haiyan The Philippines

What about Waves? Breaking waves also contribute to the total water level through wave runup/setup WAVE RUNUP is the time-varying fluctuation of water-level elevation at the shoreline due to wave breaking WAVE SETUP is the time-averaged water level rise due to wave breaking The magnitude of both runup and setup are related to offshore wave period, wave height, and shelf slope

Wave Runup

Wave Setup

Galveston Day before Ike arrived

Freshwater Input River input, esp. into bays and sounds Mississippi River discharges 200,000 700,000 cubic feet per second Rainfall

Total Water Total Water Total water level = Storm surge + Tides + Wave setup + Freshwater

No More Surge in the Saffir-Simpson Scale! (it fits like a square peg in a round hole) KATRINA (3) IKE (2) SANDY (1) ISAAC (1) CHARLEY (4)

No Such Thing as Just a Tropical Storm Louisiana State Rd. 23 near Myrtle Grove Tropical Storm Lee (2011)

Deep Water A B C Wind Wind Eye A B C 0 MSL 5O Current 100 150 200 a. Top view of Sea Surface b. Side view of Cross Section ABC

Landfall A B C Eye Wind Wind STORM SURGE A 0 50 100 150 200 B Current C MSL Mainland Barrier Island Continental Shelf a. Top view of sea surface and land b. Side view of Cross Section ABC

Understanding Surge

Factors Affecting Storm Surge Central Pressure Intensity (wind speed) Forward Speed Size Radius of Maximum Winds (RMW) Angle of Approach Width and Slope of Shelf Local features concavity of coastlines, bays, rivers, headlands, or islands

Effects of Low Pressure

Intensity (Wind Speed) 15 mph stronger

Forward Speed (Open Coast) 25 mph

Size (Radius of Max Winds)

Angle of Approach NNW NW Motion

Width and Slope of Shelf Wide shelf/ gentle slope Narrow shelf/ sharp slope

Start of shelf trapped wave up the Florida Coast

Observing and Measuring Storm Surge Tide stations (NOAA) Still water Traditionally most reliable Limited stations Stations often fail at height of event High water marks (FEMA/USGS) Perishable Traditionally best method for capturing highest surge Subjective and often include impacts of wave runup/setup Pressure Sensors (USGS) Relatively new method Deployed in advance of storm at expected location of highest surge Can contain effects of waves

High Water Mark Hoboken, New Jersey (Sandy)

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