Title: Hydrology, Hydraulics and Hydrometeorology of Floods in the Eastern United States
1Hydrology, Hydraulics and Hydrometeorology of
Floods in the Eastern United States
Baltimore Ecosystem Study LTER
Jim Smith Princeton University
2Outline and Themes
How does the 100 year flood vary over the eastern
US? Complex Terrain Central Appalachians Land
Ocean Urban Environment Basin Scale 3
Floods Warm Season Thunderstorm Systems
Smethport PA July 1942 Tropical Cyclones
Hurricane Agnes, June 1972 Winter/Spring
Extratropical Systems March 1936
3Extreme Floods and Tropical Cyclones
Hurricane Isabel 18 September 2003
Annual Flood Peak Discharge South Fork Shenandoah
River Drainage Area 1640 mi2 Record Length 78
Years 10 Year Flood 47,500 cfs 100 Year Flood
130,000 cfs
4Tropical Cyclones and Annual Flood Peaks
572 USGS Streamflow Stations. More than 75 year
record length. NOAA Atlantic Hurricane Data Base
(HURDAT).
5Isabel Rainfall (mm) Weather Research and
Forecasting (WRF) Model.
Isabel Rainfall (mm) HydroNEXRAD Rainfall
Observations
6Envelope Curve Flood Peaks in the Eastern US
7Thunderstorm Frequency Catastrophic Floods
Complex Terrain
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9Rapidan Storm 27 June 1995
10Rapidan Storm WRF Simulation
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1219 July Storms
Smethport PA 19 July 1942 30.8 inches 4 Hours
19 July 1996
1889 Rockport WVA 1942 Smethport PA 1977
Johnstown PA 1996 Redbank Creek, PA
13Moores Run, June 13, 2003
14Flood Frequency Charlotte NC
15Storm total rainfall (mm)
Storm Total Lightning (CG strikes km-2)
Storm Total Rain (mm)
7 July 2004 - Flood of Record in Dead Run
167 July 2004
Storm total rainfall (mm)
17Yellow July 7 Inundation Area Light blue FEMA
500-yr Floodplain Dark blue FEMA 100-yr
Floodplain
18Life Cycle of Warm Season Thunderstorm
Systems 1) Initiation over Blue Ridge. 2)
Propagation over Piedmont. 3) Interaction with
urban environment and land water circulation
systems.
CG lightning strikes on 13 June 2003 color
coding indicates time (hour) of occurrence.
19Summary and Conclusions
- Tropical cyclones control extreme flooding in
much of the eastern US there is pronounced
spatial heterogeneity in tropical cyclone
flooding. - Mountainous terrain (orographic precipitation
mechanisms) plays a central role in the extreme
flood hydrology of the eastern US. - Thunderstorm systems in mountainous terrain of
the eastern US have produced some of the largest
rainfall accumulations in the world for time
intervals less than 6 hours. - Envelope curve of flood peak magnitudes for the
eastern US includes numerous urban floods with
relatively short return intervals. - Climatology of urban floods is directly
linked to the climatology of warm season
thunderstorm systems.
20Weather Research and Forecasting Model - 7 July
2004 Simulations
21Conclusions from WRF Model Simulations Convergenc
e-induced spin-up along Blue Ridge Chesapeake
Bay thermal boundary plays important role in
evolution of storm system Urban Canopy has
important impacts on storm evolution No UHI
effect Aerosol effects suppression, enhancement
or redistribution.
HydroNEXRAD Storm Total Rain
WRF Storm Total Rainfall (mm)
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23CG Lightning Strikes on July 7, 2004
Initiation along Blue Ridge, propagation over
Piedmont, interaction with urban environment and
land - water boundaries (Chesapeake Bay)
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25Storm Total Lightning (CG strikes km-2)
Storm Total Lightning Strikes km-2
Storm Total Rain (mm)
- Return interval of rainfall accumulations over
Dead Run - lt 10 years at 15 minutes
- gt 300 years at 120 minutes.
26Storm Evolution 1845 - 2115 UTC on 7 July 2004
27Evolution of Storm Elements on 7 July 2004
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