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P. Eagleson (1972)
Dynamics of flood frequencyWater Resources Research, 8
I. Rodríguez‐Iturbe, Marcelo González-Sanabria, R. Bras (1982)
A geomorphoclimatic theory of the instantaneous unit hydrographWater Resources Research, 18
P. Eagleson (1978)
Climate, soil, and vegetation: 7. A derived distribution of annual water yieldWater Resources Research, 14
F. Henderson (1963)
Some properties of the unit hydrographJournal of Geophysical Research, 68
P. Eagleson, T. Tellers (1982)
Ecological optimality in water‐limited natural soil‐vegetation systems: 2. Tests and applicationsWater Resources Research, 18
J. Cordova, R. Bras (1981)
Physically based probabilistic models of infiltration, soil moisture, and actual evapotranspirationWater Resources Research, 17
I. Rodríguez‐Iturbe, J. Valdes (1979)
The geomorphologic structure of hydrologic responseWater Resources Research, 15
P. Eagleson (1978)
Climate, soil, and vegetation: 5. A derived distribution of storm surface runoffWater Resources Research, 14
V. Gupta, E. Waymire (1983)
On the formulation of an analytical approach to hydrologic response and similarity at the basin scaleJournal of Hydrology, 65
P. Eagleson (1982)
Ecological optimality in water‐limited natural soil‐vegetation systems: 1. Theory and hypothesisWater Resources Research, 18
P. Eagleson (1978)
Climate, soil, and vegetation: 2. The distribution of annual precipitation derived from observed storm sequencesWater Resources Research, 14
J. Cordova, I. Rodríguez‐Iturbe (1983)
Geomorphoclimatic estimation of extreme flow probabilitiesJournal of Hydrology, 65
C. Hebson, E. Wood (1982)
A derived flood frequency distribution using Horton Order RatiosWater Resources Research, 18
Hebson Hebson, Wood Wood (1982)
A derived flood frequency distributionWater Resour. Res., 18
P. Eagleson (1978)
Climate, soil, and vegetation: 3. A simplified model of soil moisture movement in the liquid phaseWater 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: 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 geomorphoclimatic instantaneous unit Hydrograph theory, the joint probability density function of storm duration and intensity, and Philip's representation of the infiltration process are used to derive a flood frequency distribution that could be used in regions with no streamflow records. The resulting flood frequency distribution is in analytical form containing only few climatologic and physiographic parameters of the catchment. This frequency distribution was tested against frequency distributions calculated from historic records for arid and wet climates, with good and reasonable results, respectively.
Water Resources Research – Wiley
Published: Jul 1, 1984
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