Laserfiche WebLink
<br />2-16 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />woodlands occupy another 26.3 million acres. Forest and woodland and pasture <br /> <br /> <br />and range acreages are expected to decline slightly during the next quarter <br /> <br /> <br />century, contributing to a moderate overall decline in total agricultural lands. <br /> <br /> <br />Dryland farming is the second largest type of agricultural land use in the <br /> <br /> <br />basin, exceeded only by pasture and rangelands. These nonirrigated croplands <br /> <br /> <br />are projected to increase over the next 25 years by some 2 percent from their <br /> <br /> <br />current level of nearly 90 million acres, while pasture and rangeland acreage <br /> <br /> <br />may decline substantially. <br /> <br /> <br />Irrigated cropland, estimated at 11.4 million acres in 1975, constitutes <br /> <br /> <br />about 4 percent of the present agricultural total. Irrigation is projected to <br /> <br /> <br />be applied to an additional 2.8 million acres by 1985 and to 5.9 million acres <br /> <br /> <br />by 2000, covering more than 17 million acres by the year 2000. <br /> <br /> <br />The basin's urban and transportation lands are expected to expand from the <br /> <br /> <br />present 7.4 million acres by 10 percent by 1985, and by 23 percent by the year <br />2000. Estimates of Missouri Basin land and water acreage for 1975, 1985, and <br />2000 are summarized in table 2-2. <br />WATER RESOURCES CHARACTERISTICS <br />The Missouri River Basin is, in general, well endowed with surface and <br />ground water resources. However, the occurrence and availability of water is <br />highly variable, subjecting portions of the basin to recurrent local and <br />seasonal shortages. <br />Surface Water Availability <br />Precipitation annually provides more than 500 million acre-feet of water. <br />Infiltration and evaporation deplete a large amount of this naturally occurring <br />moisture. Runoff entering the streams varies widely across the basin, ranging <br /> <br /> <br />annually from less than an inch in parts of the plains to more than 12 inches <br /> <br /> <br />in the mountains and the humid southeast. This runoff would account for an <br />