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<br />I <br />I <br />I <br />I Figure <br />8.20 <br />I <br />I <br /> 8.21 <br />I 8.22 <br />I 8.23 <br />I 8.24 <br /> 8.25 <br />I 8.26 <br />I 8.27 <br />I 8.28 <br />I 8.29 <br />,I 8.30 <br />8.31 <br />I 8.32 <br /> 10.1 <br />I 10.2 <br />I <br />I <br />I <br />- <br /> <br />CONTENTS - Continued <br /> <br /> <br />Page <br /> <br />(a) Sample PPI from a storm on January 17, 1988. Range circles <br />are drawn at 50-kilometer intervals. At this elevation <br />angle (0.50), the ground return from the Atlas Mountains <br />(southeast of the radar) is quite prominent. (b) A zoomed <br />PPI of a convective echo band in the southeast quadrant of <br />the radar on February 21, 1989, viewed with an elevation <br /> <br />angle of 1.60. ........................................... 141 <br /> <br />Time evolution of the radar return in the northern control <br />area (ZONE TEMOIN) and in the target area (ZONE CffiLE) ..... 142 <br />Time evolution of precipitation over Beni Mella! as measured <br />by radar and rain gauge (February 10, 1989) . . . . . . . . . . . . . . . . . . .. 143 <br />Echo type by synoptic situation. The four types of synoptic <br />situations are (1) postfrontal, (2) frontal, (3) prefrontal, <br />and (4) airmass convection. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 143 <br />Rain areas (km2) and water volume (m3) as a function of <br />radar reflectivity in a banded echo ........................... 144 <br />The 15 gauged basins of the Atlas Mountains for which snow <br />cover was mapped in the retrospective study. . . . . . . . . . . . . . . . . . .. 149 <br />Example Landsat band 2 image of the Atlas Mountains for <br />February 23, 1979, covering basins 2 through 11 of <br /> <br />figure 8.25 ............................................. 150 <br /> <br />Example A VHRR visible band image of Morocco for <br />February 23, 1979 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 150 <br />Plot of proportion snow-covered area versus time for basin 8 <br />of figure 8.25, Ait Tamlilt, for the 1978-79 and 1981-82 <br /> <br />seasons ............................................... 151 <br /> <br />Area-elevation curve for the Tillouguit basin, showing <br />determination of mean hypsometric elevations for each <br />of the three elevation bands used to model snowmelt runoff ........ 151 <br />Schematic of the Martinec-Rango Snowmelt Runoff Model ....... . . . " 152 <br />Plot of simulated and measured streamflows for the <br />Tillouguit basin in the 1979 snowmelt season. . . . . . . . . . . . . . . . . . .. 152 <br />Plot of simulated and measured streamflows for the <br />Tillouguit basin for March 1986 ............................. 153 <br />Map of watershed, stream gauges, and dam locations within <br />the Oum Er Rbia River basin . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 191 <br />Schematic representation of the Oum Er Rbia water <br />management system showing diversions for turbines, . <br />irrigation, and municipal industrial water. Quantities of <br />installed hydroelectric capacity (MW), reservoir elevation, <br />and capacity (m3) are shown at each diversion. . . . . . . . . . . . . . . . . .. 192 <br /> <br />xxv <br />