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By Shapley H.

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Additional info for A Short Period Cepheid with Variable Spectrum (1916)(en)(5s)

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The dimensions of the channel can only be explained by a single discharge of a given frequency when either the temporal fluctuation in discharge is low, or the particular channel dimension is insensitive to flow variations. In a similar vein, Wolman & Gerson (1978) argued that the effectiveness of an event reflects the morphological changes caused by both erosion and deposition, as well as the associated sediment transport that occurs during a flood event. In semi-arid channels, forms tend to represent the last major flood and recovery periods are relatively long (up to 100 years: Fig.

F ERNANDES , N. F. & D IETRICH , W. F. 1997. Hillslope evolution by diffusive processes: the time scale for equilibrium adjustments. Water Resources Research, 33, 1307– 1318. F LEMINGS , P. B. & J ORDAN , T. E. 1989. A synthetic stratigraphic model of foreland basin development. Journal of Geophysical Research, 94, 3851– 3866. F OURNIER , F. 1960. Climat et Erosion. La Relation entre l’Erosion du Sol par l’eau et les Pre´cipitations Atmosphe´riques. Presses Universitaires de France, Paris. F RASER , G.

G UIDON , R. & G OLDIN , T. 2004. Footwall topographic development during continental extension. Journal of Geophysical Research, 109, F03001. D ENSMORE , A. , D AWERS , N. , G UPTA , S. & G UIDON , R. 2005. What sets topographic relief in extensional footwalls? Geology, 33, 453– 456. D ENSMORE , A. , A LLEN , P. A. & D AWERS , N. H. 2007a. Transient landscapes at fault tips. 1029/2006JF000560. D ENSMORE , A. , A LLEN , P. A. & S IMPSON , G. 2007b. Development and response of a coupled catchment– fan system under changing tectonic and climatic forcing.

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A Short Period Cepheid with Variable Spectrum (1916)(en)(5s) by Shapley H.


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