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    Balanced Design Storm UH, Rational, and Regression Equation Methods 

    Source: Journal of Hydrologic Engineering:;1997:;Volume ( 002 ):;issue: 003
    Author(s): T. V. Hromadka II
    Publisher: American Society of Civil Engineers
    Abstract: In practice, runoff peak flow rates are typically estimated by the rational method, a design storm unit hydrograph (UH) method, or a statistical regression equation. In this technical note, the balanced design storm UH ...
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    Stochastic Evaluation of Rainfall-Runoff Prediction Performance 

    Source: Journal of Hydrologic Engineering:;1997:;Volume ( 002 ):;issue: 004
    Author(s): T. V. Hromadka II
    Publisher: American Society of Civil Engineers
    Abstract: Given a set of realizations of error data (i.e., the difference between model runoff estimates and stream gauge data) from rainfall-runoff hydrologic models, it is possible to generate a set of error transfer function ...
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    Checking Flood Frequency Curves Using Rainfall Data 

    Source: Journal of Hydraulic Engineering:;1989:;Volume ( 115 ):;issue: 004
    Author(s): T. V. Hromadka, II; R. J. Whitley
    Publisher: American Society of Civil Engineers
    Abstract: There is no agreement on the best way to develop flood frequency curves and synthesize runoff peak flow rate data, and no precise procedure which applies to all cases of flood frequency statistics. Consequently it is prudent ...
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    Complex Polynomial Approximation of the LaPlace Equation 

    Source: Journal of Hydraulic Engineering:;1984:;Volume ( 110 ):;issue: 003
    Author(s): T. V. Hromadka, II; Gary L. Guymon
    Publisher: American Society of Civil Engineers
    Abstract: A method of approximating the solution of the Laplace equation in two‐dimensions is presented. The numerical approach is to determine a complex variable polynomial which satisfies the specified boundary conditions along a ...
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    Rational-Method Equation and HEC TD-15 

    Source: Journal of Irrigation and Drainage Engineering:;1996:;Volume ( 122 ):;issue: 001
    Author(s): T. V. Hromadka II; R. J. Whitley
    Publisher: American Society of Civil Engineers
    Abstract: The rational-method equation for estimating peak flow rates for storm-water runoff is derived from the balanced-design storm unit hydrograph approach presented in the U.S. Army Corps of Engineers HEC Training Document 15. ...
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    Closure to “<i>Kinematic Wave Routing and Computational Error</i>” by T. V. Hromadka II and J. J. DeVries (February, 1988, Vol. 114, No. 2) 

    Source: Journal of Hydraulic Engineering:;1990:;Volume ( 116 ):;issue: 002
    Author(s): T. V. Hromadka, II; J. J. DeVries
    Publisher: American Society of Civil Engineers
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    Comparison of Overland Flow Hydrograph Models 

    Source: Journal of Hydraulic Engineering:;1987:;Volume ( 113 ):;issue: 011
    Author(s): T. V. Hromadka, II; R. H. McCuen; C. C. Yen
    Publisher: American Society of Civil Engineers
    Abstract: The diffusion equation is a simplification of the two‐dimensional continuity and momentum equations. This simpler dynamic model of two‐dimensional hydraulics affords the hydrologist a means to quickly estimate floodflow ...
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    Cumulative Departure Model of the Cryosphere During the Pleistocene 

    Source: Journal of Cold Regions Engineering:;2014:;Volume ( 028 ):;issue: 003
    Author(s): T. V. Hromadka II; H. D. McInvale; B. Gatzke; M. Phillips; B. Espinosa
    Publisher: American Society of Civil Engineers
    Abstract: A mathematical model is developed to describe changes in ice volume in the cryosphere. Modeling the cryosphere may be useful in assessing future climate impacts currently captured by global circulation models (GCMs) by ...
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    Mathematical Model of Cryospheric Response to Climate Changes 

    Source: Journal of Cold Regions Engineering:;2013:;Volume ( 027 ):;issue: 002
    Author(s): T. V. Hromadka II; M. Jaye; M. Phillips; T. Hromadka III; D. Phillips
    Publisher: American Society of Civil Engineers
    Abstract: This paper focuses on the development of simplified mathematical models of the cryosphere which may be useful in further understanding possible global climate change impacts and in further assessing future impacts captured ...
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