The Spectral Power Density and Shadowing Function of a Glacial Microrelief at the Decimetre Scale
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Abstract Longitudinal profiles of roches moutonnées have been measured once every centimetre over a total length of more than 100 m. Only wavelengths in the range 3.6 cm < λ < 40 cm have been kept and analysed. Levels and their slopes have a symmetrical, non-Gaussian distribution. The spectral power density varies roughly as γ 0 ν–n (ν ═ wavenumber ═ 1/λ); n being the same for all the profiles (n ═ 2.36) and γ 0 being dependent on the studied area. No significant difference has been found for the shadowing function of the different studied areas. It differs consistently from Smith’s theoretical function.
2020 ◽
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pp. 651-657
2019 ◽
Vol 20
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pp. 3486
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1973 ◽
Vol 35
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pp. 331-332
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1972 ◽
Vol 33
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pp. 113-115
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2011 ◽
Vol 26
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pp. 1081-1087
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2017 ◽
Vol 57
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pp. 012101
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2003 ◽
Vol 1
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pp. 41-44
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