Abstract
Streamflow records are one of the bases used in the design and operation of complex water resource systems. Unfortunately records available from many streams are of insufficient length and no streamflow data have been recorded for some streams. Consequently estimates of unrecorded flows are often required for hydrolgic studies. To estimate data at a site for which some records exist, relationships may be established between the existing record and records from nearby sites, (3). The more difficult problem of estimating streamflow data at sites for which no records exist is the topic of this chapter.
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References
Fuller, G. A., 1978, Generation of Ungauged Streamflow Data, J. Hydraul. Div., Am. Soc. Civil Engr., Vol. 104, No. HY3.
Fuller, G. A. and N. E. Fuller, 1974, Inconsistent Matrices in Estimating Ungauged Streamflow Data, Water Resour. Res., Vol. 10, No. 6, pp. 1949–1950.
Fuller, G. A. and H. M. Hill, 1970, Data Preparation for Great Lakes Studies, Proc. 1970 Conf. of Intl. Assoc. for Great Lakes Research, Buffalo, N.Y., Mar. 31 to Apr. 3, pp. 997-1003.
Richardson, C. H., 1944, An Introduction to Statistical Analysis, Harcourt, Brace, and Co., N.Y., pp. 277–305.
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© 1983 Martinus Nijhoff Publishers, The Hague
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Fuller, G.A. (1983). Generation of Runoff Data for Ungauged Streams. In: Guggino, E., Rossi, G., Hendricks, D. (eds) Operation of Complex Water Systems. NATO ASI Series, vol 58. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-6807-3_33
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DOI: https://doi.org/10.1007/978-94-009-6807-3_33
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