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National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium Jim Noel Service Coordination Hydrologist Robin Belton-Gerhardt Hydrologist March 22, 2013

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Page 1: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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NOAA/NWSOhio River Forecast Center

Hydrology 1913 to 2013.Ohio State Severe Weather

Symposium

NOAA/NWSOhio River Forecast Center

Hydrology 1913 to 2013.Ohio State Severe Weather

Symposium

Jim NoelService Coordination Hydrologist

Robin Belton-GerhardtHydrologist

March 22, 2013

Page 2: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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OutlineOutline

Hydrology of 1913 Duration of 1913 flood Magnitude of 1913 flood Big floods in the Ohio Valley 1913 in 20131913, 1997 and 2010 in 2013 Today’s Advances in Hydrology

Page 3: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Hydrology of 1913Hydrology of 1913 There was no snowpack prior to the event Soil conditions were wet leading into the event Streamflow conditions were not really elevated 1913 was an extreme event but also had a lot of

classic historic event characteristics Most of the intense rain fell in a few days Runoff rates were very high, close to 1, complete

runoff Rivers responded fast to the runoff Systems failed as Mother Nature exceeded the

capabilities of the system (both natural and man-made)

Page 4: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Hydrology of 1913Hydrology of 1913 River gages where 1913 flood of record still

stands.

Page 5: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Duration of Flooding from 1913Duration of Flooding from 1913 Flood happened fast in the faster responding

upper Ohio River and Great Lakes basins.

LegendDays Above Flood Stage

1-33-10

10-2020-30

>30

Page 6: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Magnitude of Flooding from 1913Magnitude of Flooding from 1913 Minor flooding begins to appear in northern Ohio ahead

of the main storm

Page 7: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Magnitude of Flooding from 1913Magnitude of Flooding from 1913 Flood expands across northern Indiana to northern Ohio

and western Pennsylvania in faster responding areas.

Page 8: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Magnitude of Flooding from 1913Magnitude of Flooding from 1913 Significant flooding occurring rapidly in faster responding

tributaries

Page 9: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Magnitude of Flooding from 1913Magnitude of Flooding from 1913 Widespread major flooding is occurring across the northern

Ohio Valley into the Lake Erie drainage areas

Page 10: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Magnitude of Flooding from 1913Magnitude of Flooding from 1913 Significant flooding subsiding in upstream tributaries but

continues in downstream tributaries into Ohio River.

Page 11: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Magnitude of Flooding from 1913Magnitude of Flooding from 1913 Flooding is shifting from the fast responding to slower

responding rivers by March 28, 2013

Page 12: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Magnitude of Flooding from 1913Magnitude of Flooding from 1913 Flooding now focused on lower Wabash, lower White

basins of Indiana into Ohio River.

Page 13: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Magnitude of Flooding from 1913Magnitude of Flooding from 1913 By April 1 the flood is now mainly in the Ohio River and heading downstream.

It usually takes about a week for the water to move down the Ohio River.

Page 14: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Big floods in the Ohio ValleyBig floods in the Ohio Valley Big floods are common in the Ohio Valley Do these sound familiar: 1913, 1927, 1937, 1959, 1964, 1997, 2005,

2008, 2010, 2011 to name a few. Many more. Next one is 201?Why? Crossroads of the jet stream. Ohio River Forecast Center is one of the busiest in the country,

usually in top three of 13 RFCs. Flooding occurs in most months of the year. Most big floods have a similar look! Most meteorologists and hydrologists focus on the 500 mb trough.

However, OHRFC research suggests the Southeast Ridge is even more important – like a ball hitting a wall!

Page 15: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Big floods in the Ohio ValleyBig floods in the Ohio Valley1913 500 hPa

Composite2010 500 hPa

1997 500 hPa

ATL= 585 ATL= 585

ATL= 585 ATL= 582

Page 16: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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1913 flood in 20131913 flood in 2013 Youngstown, Ohio crest would be lower and

faster with local water getting in faster. Also, Army Corps of Engineers holds water in their projects and release later for longer recession.

Page 17: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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1913 flood in 20131913 flood in 2013 Zanesville, Ohio crest would be substantially

lower as upstream projects of the Army Corps of Engineers and Muskingum Conservancy District hold water and release later for longer recession.

Page 18: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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1913 flood in 20131913 flood in 2013 Columbus, Ohio crest would be similar or

possibly slightly higher. However, due to levee failures (1913) and other complexities, confidence is low at this point.

Page 19: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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1913 flood in 20131913 flood in 2013 Dayton, Ohio crest would be substantially lower

as upstream projects of the Miami Conservancy District hold water and release later for longer recession. Flood Stage would not occur.

Page 20: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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1913 flood in 20131913 flood in 2013 Fort Wayne, Indiana crest would be slightly

higher and later with faster recession. This is likely a combination of urbanization and water getting into system faster.

Page 21: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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1913 flood in 20131913 flood in 2013 Terre Haute, Indiana crest would be lower and

faster with similar recession. Local water gets into system slightly faster. Much of the landscape remains agriculture over this time.

Page 22: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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1913 flood in 20131913 flood in 2013 Indianapolis, Indiana crest would be lower with

double crest from local water, then upstream water arriving. Urbanization is responsible for initial crest. Recession is slower.

Page 23: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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1913, 1997 and 2010 flood in 20131913, 1997 and 2010 flood in 2013 So, can we have worse floods in terms of rainfall

than the 1913 flood?Answer is YES! If so, what would some other recent floods, such

as the 1997 Kentucky flood and 2010 Nashville flood, look like today?

19138-10+ inches

19979-11+ inches

201010-15+ inches

Page 24: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Columbus, Ohio – Convective extreme events such as the 2010 event in Nashville of up to 15+” of rain would cause extreme rises. Exact crests would be driven by how the system can maintain itself. Crests likely lower than shown here because things could fail.

1913, 1997 and 2010 flood in 20131913, 1997 and 2010 flood in 2013

Page 25: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Dayton, Ohio – Flooding would be far less than in 1913 due to the impressive system built. 1913 today would be similar to 1997 today with 2010 being a more impressive system, but still well below 1913.

1913, 1997 and 2010 flood in 20131913, 1997 and 2010 flood in 2013

Page 26: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Today’s Advances in HydrologyToday’s Advances in Hydrology Flood systems are in place, as in parts of the Miami

and Muskingum systems. Awareness is much better. Forecasting is now available with decent lead times. River modeling continues to improve. Ensemble and probabilistic forecasting are advancing. Flood mapping is expanding. Hydrology is in the rapid growth period much like

meteorology was in 1985.

Page 27: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Today’s Advances in HydrologyToday’s Advances in HydrologyRiver Ensemble Forecasting System

http://www.erh.noaa.gov/mmefs

Page 28: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Today’s Advances in HydrologyToday’s Advances in HydrologyRiver Ensemble Forecasting System

http://www.erh.noaa.gov/mmefs

Page 29: National Weather Service Protecting Lives and Property NOAA/NWS Ohio River Forecast Center Hydrology 1913 to 2013. Ohio State Severe Weather Symposium

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Questions!Questions!

[email protected]

NOAA/NWS/OHRFC Service Coordination Hydrologist

THANKS!