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- W1587972913 abstract "This chapter discusses some research problems associated with the scaling of land-surface hydrologic processes involved in the land-surface water-and-energy budget. As pointed out by Dubayah, Wood, and Lavallee (1996), the term “scaling” has come to have multiple definitions, depending not only on the general discipline (e.g., hydrology, meteorology, geography, physics) but also on the application within a discipline. Dubayah et al. (1996) refer to a process as exhibiting scaling “if no characteristic length scale exists; i.e. the statistical spatial properties of the field do not exhibit scale-dependent behavior.” Bloschl and Sivapalan (1995) refer to scaling as the transfer of information between different spatial (or temporal) lengths. The “transfer of information” may consist in mathematical relationships, statistical relationships, or observations describing physical phenomena. This definition is consistent with that of Dubayah et al. (1996), albeit more qualitative. The term “upscaling” is often used by the remote-sensing community to describe going from observations on a small spatial (or temporal) scale to observations on larger scales, whereas “downscaling” consists in going from large-scale observations to smaller scales." @default.
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- W1587972913 date "1998-08-13" @default.
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- W1587972913 title "Scale Analyses for Land-Surface Hydrology" @default.
- W1587972913 doi "https://doi.org/10.1017/cbo9780511551864.002" @default.
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