Search results
Results From The WOW.Com Content Network
Runoff patterns across the Colorado River Basin reflect this; most of the perennial tributaries originate in the Upper Basin, while tributaries in the Lower Basin are either ephemeral (such as the Little Colorado River) or highly seasonal (such as the Gila and Salt rivers). [57]
Runoff is the flow of water across the earth, and is a major component in the hydrological cycle. Runoff that flows over land before reaching a watercourse is referred to as surface runoff or overland flow. Once in a watercourse, runoff is referred to as streamflow, channel runoff, or river runoff. Urban runoff is surface runoff created by ...
The river's first diversion is here at its headwater. The Grand Ditch redirects water from the Never Summer Mountains, which would have flowed into the Colorado River, to instead flow across the divide through La Poudre Pass to irrigate farmland to the east. Near the source of the Colorado River in Rocky Mountain National Park, Colorado
The following is a tree demonstrating the points at which the major and minor tributaries of the Colorado River branch off from the main river and from each other. (Source-upstream)
Water from the Colorado River is diverted near Yuma, Arizona, into the 82-mile (132 km) All-American Canal. The canal runs west along the Mexican border and then north into 1,700 miles (2,700 km) of irrigation channels that crisscross the farms. [30] Gravity carries the agricultural runoff downhill through the New and Alamo rivers to the lake. [30]
"Six out the seven states within the Colorado River Compact rank in the top 10 of most water stressed states in the United States." The Atlas finds that across the globe, 25 countries experience ...
The Colorado River Upper Basin, comprised of Colorado, Wyoming, Utah and New Mexico, and the Lower Basin, made up of California, Arizona and Nevada, have been quarreling for months over seemingly ...
Runoff routing is a procedure to calculate a surface runoff hydrograph from rainfall. Losses are removed from rainfall to determine the rainfall excess which is then converted to a hydrograph and routed through conceptual storages that represent the storage discharge behaviour of overland and channel flow.