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P. Eagleson (1972)
Dynamics of flood frequencyWater Resources Research, 8
P. Eagleson (1978)
Climate, soil, and vegetation: 2. The distribution of annual precipitation derived from observed storm sequencesWater Resources Research, 14
P. Eagleson (1978)
Climate, soil, and vegetation: 1. Introduction to water balance dynamicsWater Resources Research, 14
P. Eagleson (1978)
Climate, soil, and vegetation: 3. A simplified model of soil moisture movement in the liquid phaseWater Resources Research, 14
I. Gradshteyn, I. Ryzhik, A. Jeffrey, Y. Geronimus, M. Tseytlin, Y. Fung (1966)
Table of Integrals, Series, and ProductsJournal of Lubrication Technology, 98
W. Grayman, P. Eagleson (1969)
Streamflow record length for modelling catchment dynamics
J. Philip (1969)
Theory of Infiltration, 5
P. Eagleson (1978)
Climate, soil, and vegetation: 6. Dynamics of the annual water balanceWater Resources Research, 14
P. Eagleson (1978)
Climate, soil, and vegetation: 4. The expected value of annual evapotranspirationWater Resources Research, 14
The Philip infiltration equation is integrated over the duration of a rainstorm of uniform intensity to give the depth of point surface runoff from such an event on a natural surface in terms of random variables defining the initial soil moisture, the rainfall intensity, and the storm duration. In a zeroth‐order approximation the initial soil moisture is fixed at its climatic space and time average, whereupon by using exponential probability density functions for storm intensity and duration, the probability density function of point storm rainfall excess is derived. This distribution is used to define the annual average depth of point surface runoff and to derive the flood volume frequency relation, both in terms of a set of physically meaningful climate‐soil parameters.
Water Resources Research – Wiley
Published: Oct 1, 1978
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