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�1 <br />INTRODUCTION <br />Experience teaches that it is not wise to depend upon rainfall where the amount is less than 20 <br />inches annually. The isohyetal or mean rainfall line of 20 inches ... in a general way... it may <br />be represented by the one hundredth meridian. [In this region] agriculturalists will early resort <br />to irrigation. John Wesley Powell, 1878 <br />The 100th meridian is a defining geographic feature in the United States that marks <br />important transitions for land, water, and life. In the Great Plains, this north -south line <br />(immediately east of Cozad, Nebraska) transects the corridor of the central Platte River Valley of <br />Nebraska, the subject of this report. The river is emblematic of the human and ecological <br />complexities of policy, science, and management for a dryland river (Figure 1 -1). The river was <br />named the Platte River, French for "flat river ", on June 2, 1739, by two French explorers who <br />were searching for a route from Illinois to Santa Fe, New Mexico (Sheldon 1913). <br />. The Platte River's two great branches, the North Platte and the South Platte, rise in the <br />Rocky Mountains in the West and join in western Nebraska to the west of the 100th meridian <br />(Figure 1 -2). The river flows 310 mi (about 500 km) through Nebraska across the meridian to a <br />confluence with the Missouri River. The Platte River delivers the runoff of its 86,000 -mi2 <br />(223,000 -km2) drainage area, largely the result of precipitation in the high western mountains, to <br />an extensive system of water control for the highly productive agricultural area in the plains. <br />The river is more than a conduit for water, however; along its course, it creates an aquatic and <br />riparian ecosystem that provides wildlife habitat unlike habitats found outside the river valley. <br />The river corridor, within the Central Flyway of North America, provides habitat for migratory <br />and breeding birds, including three endangered or threatened species: the whooping crane (Gnus <br />americans), the piping plover (Charadrius melodus), and the interior least tern (Sterna <br />antillarum athalassos). The broad shallow waters of the Platte near its confluence with the <br />Missouri River constitute an important habitat for at least one endangered species of fish: the <br />pallid sturgeon (Scaphirhynchus albus). <br />The infrastructure investments that made irrigated agriculture and urban water supply <br />possible in the Platte River Basin have substantially altered the hydrologic regime of the Platte <br />River. During the 20th century in the Platte River Basin, construction of storage reservoirs and <br />diversion dams and installation of wells to tap groundwater supported the economic vitality of <br />the region. The structures continue to provide flood reduction, water supply, hydroelectricity, <br />and recreational benefits. By controlling and diverting water flows, however, the dams altered. <br />the stream flows, and that caused widespread environmental changes. A major habitat change <br />involved the expansion of woodland and the narrowing of river channels. Whooping cranes, <br />piping plovers, and interior least terns, whose populations were already declining because of <br />• other factors, prefer more sparsely vegetated, open, sandy areas near shallow water. <br />15 <br />