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<br /> 1.5 <br /> A. <br /> 1.0 <br /> 0.5 <br /> 0.0 <br />c:: <br />.2 -0.5 <br />Ei <br />'0. <br />.~ -1.0 <br />a. <br />-0 <br />.. <br />N 1.5 <br />'5 <br />lu B. <br />-0 <br />c:: <br />'" 1.0 <br />Cii <br /> 0.5 <br /> 0.0 <br /> -0.5 <br /> -1.0 <br /> 0 0 <br /> 0 ~ <br /> '" '" <br /> <br />July - Sept <br /> <br /> <br />Nov - Mar <br /> <br /> <br />o <br />'" <br />'" <br /> <br />o <br />'" <br />'" <br />~ <br /> <br />o <br />..,. <br />'" <br />~ <br /> <br />o <br />on <br />'" <br /> <br />o <br />co <br />'" <br /> <br />o <br />.... <br />'" <br /> <br />o <br />'" <br />'" <br /> <br />o <br />o <br />o <br />'" <br /> <br />o <br />ex> <br />'" <br /> <br />Figure 4. Standardized seasonal precipitation for the Grand Canyon region from 1904 <br />through 1998 based on data from 14 weather stations (table 3). A. Summer (July through <br />September). B. Winter (November through March). <br /> <br />and data from gaging stations on small drainages. <br />Data are available for sediment yield per year per <br />unit area for 25 reservoirs (fig. 6). In addition to the <br />reservoir sedimentation data, we assembled <br />sediment yield data from 12 gaging stations on <br />small watersheds in the region (table 4). Data from <br />eight of these watersheds are previously <br />unpublished and come from gaging stations <br />operated by Peabody Coal Company on Black <br />Mesa (D.R. Hardey, unpublished data, 1999). The <br />data were combined despite the fact that some <br />stations have data predominantly from the period <br />1948-1979 and others from Black Mesa were <br />collected in the 1980s and 1990s in a period of <br />higher rainfall (figs. 3-5). In addition, the Hains and <br /> <br />others (1952) data represent total sediment load <br />whereas suspended load was measured at the <br />gaging stations. <br />We combined the reservoir sedimentation data <br />with the annual sediment yields from gaging <br />stations in the region, excluding the mainstem <br />Colorado River (table 4). Fitting a power function <br />to these data (fig. 6), we obtained <br /> <br />Q, = 193 . A 1.04, R2 = 0.86, (3) <br /> <br />where Q, = sediment yield (Mg/yr), A = drainage <br />area (km2), and n = 37. We used equation (3), <br />termed the data regression equation, to estimate <br />sediment yields from all 768 tributaries, summed by <br />geomorphic reach (table 6). <br /> <br />STREAMFLOW SEDIMENT YIELD 11 <br />