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By Ven Chow, David Maidment, Larry Mays

This article is designed for a hydrologist, civil, or agricultural engineer. The textual content offers an built-in method of hydrology, utilizing the hydrologic/system or keep watch over quantity as a mechnism for studying hydrologic difficulties.

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Chow, V. , Open-channel Hydraulics, McGraw-Hill, New York, 1959. Emmett, W. , Overland flow, in Hillslope Hydrology, ed. by M. J. Kirkby, Wiley, Chichester, England, pp. 145-176, 1978. Fahien, R. , Fundamentals of Transport Phenomena, McGraw-Hill, New York, 1983. Fox, R. , and A. T. , Wiley, New York, 1985. Freeze, R. , and J. A. Cherry, Groundwater, Prentice-Hall, Englewood Cliffs, N J . , 1979. French, R. , Open-channel Hydraulics, McGraw-Hill, New York, 1985. Giancoli, D. C , General Physics, Prentice-Hall, Englewood Cliffs, N J .

5 billion. The annual population increase during the preceding decade was about 2 percent. 8 m3/day (1800 gal/day) per capita including public water supplies and water withdrawn for irrigation and industry. Assume that 47,000 km3 of surface and subsurface runoff is available for use annually. 5. Calculate the global average precipitation and evaporation (cm/yr). 6. Calculate the global average precipitation and evaporation (in/yr). 1. Take three hydrologic systems with which you are familiar. For each, draw the system boundary and identify the inputs, outputs, and working media.

Which states that the volumetric inflow rate and outflow rate are equal; that is, /(O = Q{t). A steady flow is one in which the velocity at every point in the flow is constant in time. A simple way of thinking about this is to imagine taking a "snapshot" of the flow now, and again five minutes later; if the the flow is steady, the two snapshots will be identical. 6) J —oo When this condition does not hold, the system is open. The hydrologic cycle is a closed system for water, but the rainfall-runoff process on a watershed is an open system, because not all the rainfall becomes runoff; some is returned to the atmosphere through evaporation.

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