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Автор Yang, Chih Ted
Автор Stall, John B.
Дата выпуска 1971
dc.description The Strahler stream order assigned to a particular stream segment depends on the scale of the topographic map used in ordering the stream network. However, the Horton‐Strahler bifurcation ratio of stream number, stream length ratio, and stream concavity are found to be independent of map scale. The coefficients in Horton's laws obtained from a map system of one scale can be transferred to a map system of another scale if the stream order difference between the two map systems is given. Yang's theoretical and equilibrium longitudinal stream bed profiles are shown to be independent of map scale and can be compared favorably with an actual profile obtained from a topographic map of any scale.
Формат application.pdf
Копирайт Copyright 1971 by the American Geophysical Union.
Название Note on the Map Scale Effect in the Study of Stream Morphology
Тип shortCommunication
DOI 10.1029/WR007i003p00709
Electronic ISSN 1944-7973
Print ISSN 0043-1397
Журнал Water Resources Research
Том 7
Первая страница 709
Последняя страница 712
Выпуск 3
Библиографическая ссылка Horton, R. E., Erosional development of streams and their drainage basins; hydrophysical approach to quantitative morphology, Geol. Soc. Amer. Bull., 563, 275–370, 1945.
Библиографическая ссылка Scheidegger, A. E., Effect of map scale on stream orders, Bull. Int. Ass. Sci. Hydrol., 113, 56–61, 1966.
Библиографическая ссылка Stall, John B., C. T.Yang, Hydraulic geometry of 12 selected stream systems of the United StatesWater Resour. Cent. Res. Rep. 32University of Illinois, Urbana, 1970.
Библиографическая ссылка Strahler, A. N., Quantitative analysis of watershed geomorphology, Trans. Amer. Geophys. Union, 386, 913–920, 1957.
Библиографическая ссылка Yang, C. T., Potential energy and stream morphology, Water Resour. Res., 7311, 322, 1971.

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