Estimating the Magnitude of Peak Flows for Streams in Kentucky for Selected Recurrence Levels

Estimating the Magnitude of Peak Flows for Streams in Kentucky for Selected Recurrence Levels PDF Author: Glenn Hodgkins
Publisher:
ISBN:
Category : Flood forecasting
Languages : en
Pages : 80

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Book Description

Estimating the Magnitude of Peak Flows for Streams in Kentucky for Selected Recurrence Levels

Estimating the Magnitude of Peak Flows for Streams in Kentucky for Selected Recurrence Levels PDF Author: Glenn Hodgkins
Publisher:
ISBN:
Category : Flood forecasting
Languages : en
Pages : 80

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Book Description


Estimating the Magnitude of Peak Flows for Streams in Kentucky for Selected Recurrence Levels

Estimating the Magnitude of Peak Flows for Streams in Kentucky for Selected Recurrence Levels PDF Author: Glenn Hodgkins
Publisher:
ISBN:
Category : Flood forecasting
Languages : en
Pages : 68

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Estimating the Magnitude of Peak Flows for Streams in Maine for Selected Recurrence Intervals

Estimating the Magnitude of Peak Flows for Streams in Maine for Selected Recurrence Intervals PDF Author: Glenn Hodgkins
Publisher:
ISBN:
Category : Stream measurements
Languages : en
Pages : 56

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Book Description
This report gives estimates of, and presents techniques for estimating, the magnitude of peak flows for streams in Maine for recurrence intervals of 2, 5, 10, 25, 50, 100, and 500 years. A flow chart in this report guides the user to the appropriate estimates and (or) estimating technique for a site on a specific stream.

Estimating the Magnitude of Peak Flows at Selected Recurrence Intervals for Streams in Idaho

Estimating the Magnitude of Peak Flows at Selected Recurrence Intervals for Streams in Idaho PDF Author:
Publisher: DIANE Publishing
ISBN: 1428910948
Category :
Languages : en
Pages : 62

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Estimating the Magnitude of Peak Flows at Selected Recurrence Intervals for Streams in Idaho

Estimating the Magnitude of Peak Flows at Selected Recurrence Intervals for Streams in Idaho PDF Author: Charles Berenbrock
Publisher:
ISBN:
Category : Flood forecasting
Languages : en
Pages :

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Techniques for Estimating Peak-flow Magnitude and Frequency Relations for South Dakota Streams

Techniques for Estimating Peak-flow Magnitude and Frequency Relations for South Dakota Streams PDF Author: Steven Kent Sando
Publisher:
ISBN:
Category : Stream measurements
Languages : en
Pages : 56

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Technique for Estimating Magnitude and Frequency of Peak Flows in Delaware

Technique for Estimating Magnitude and Frequency of Peak Flows in Delaware PDF Author: Jonathan J. A. Dillow
Publisher:
ISBN:
Category : Floodplain management
Languages : en
Pages : 38

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Regression Equations for Estimating Flood Flows for the 2-, 10-, 25-, 50-, 100-, and 500-year Recurrence Intervals in Connecticut

Regression Equations for Estimating Flood Flows for the 2-, 10-, 25-, 50-, 100-, and 500-year Recurrence Intervals in Connecticut PDF Author: Elizabeth A. Ahearn
Publisher:
ISBN:
Category : Flood forecasting
Languages : en
Pages : 72

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Techniques for Estimating Magnitude and Frequency of Peak Flows for Pennsylvania Streams

Techniques for Estimating Magnitude and Frequency of Peak Flows for Pennsylvania Streams PDF Author: Marla H. Stuckey
Publisher:
ISBN:
Category : Flood control
Languages : en
Pages : 56

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Flood Flow Estimation for Stream Restoration Applications in Kentucky Streams

Flood Flow Estimation for Stream Restoration Applications in Kentucky Streams PDF Author: Adam Mark Connelly
Publisher:
ISBN:
Category :
Languages : en
Pages : 170

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Book Description
The following study develops flood frequency curves based on drainage area for various physiographic hydrologic regions in Kentucky. The log-Pearson Type III distribution is used to obtain the flow magnitudes corresponding to select recurrence interval discharges of interest. Stream gages with an annual peak records greater than 10 years and drainage areas less than 1000 square miles are examined to analyze stream corridors that are frequently considered for stream restoration projects. The developed flood frequency curves are used to compare the variation in magnitude between select recurrence interval flood flows.