Laserfiche WebLink
<br />DO;J03S <br /> <br />/ <br /> <br /> <br />CHAPTER I <br /> <br />DROUGHT INFORMATION NEEDED <br /> <br />THE I)ROUGBT COMES <br /> <br />Except for a n4rr0.... coastal strip in the Pacific <br />Northwest, the wes,tern. states have an arid climate ' <br />and largely depend ;on winter snowfall in the higher <br />mountains for water supply, Most irrigation projects <br />and metropolitan ""as depend on reservoirs to store <br />the spring runoff felr later use during the long dry <br />summer. The larger reservoirs are designed to hold <br />water from wet petiods for use during dry periods <br />several years later, ~ut each dry year brings more dry <br />reservoirs and increases the probability of severe <br />water shortage. <br /> <br />In the winter of 1975-76, the normal eastward <br />movement of stormj, coming inland from the Pacific <br />was so often blocked by an extraordinarily stable high <br />pressure ridge off t.e California eoast that precipita- <br />tion amounts were near record lows in California and <br />the states to its east, The early winter months were <br />much wetter in the l'acific Northwest, but by the new <br />year the high pre$ure ridge was often extending <br />further north and p1\':"ipitation amounts were running <br />below normal throu~h the more northern tier of states <br />as well. During tha~,winter and the following summer, <br />the most severe eff~s were felt by those depending <br />on a dry land famjing or a range economy and on <br />municipalities that i did not have enough reservoir <br />storage or ground"iater resources to provide carry. <br />over storage from Ejarlier, wetter years. <br /> <br />Tropical stornls caused some unusual rainfall <br />amounts in the areljs near the Mexican border in the <br />summer of 1976, b\1t by early winter, it was quite <br />evident that the sta.le high pressure conditions of the <br />previous winter hajl not only returned but that the <br />ridge was even mOrl> persistent and extended further <br />north than during the previous winter. Normal <br />snowpacks were riot accumulating in any of the <br />western mountains ivithtypicalamounts ranging from <br />30 to 50 percent of ~ver.ge. Streamflow forecasts for <br />many areas were 2Oito 30 percent of average. At many <br />locations, these amdunta were the least they had been <br />in as much as 100 years of record. <br /> <br />By December,' the ski resorts were suffering <br />severe losses, wintllr grain growers knew they would <br />be fortunate to ge~ any kind of crop, and livestock <br />ranchers were seIl{ng extra animals in an effort to <br /> <br />save enough feed for their basic herd. The more <br />severely impacted municipalitiea were by Marcb <br />rationing water or charging severe penalties for <br />wasteful use, Irrigators and municipalities throughout <br />the west knew that unless a change in the, weather <br />pattern brought more precipitation, aIi would be <br />experiencing severe water shortage by the end of the <br />summer. Percentages of normal precipitation did <br />generally increase somewhat through the late spring <br />and summer, but shortages remained severe. In fact, <br />it was largely carryover storage. in th.e larger <br />reservoirs and groundwater mining that saved the <br />day. <br /> <br />To the east, simultaneous severe drought <br />conditions were experienced during the winter and <br />spring in the upper midwest, centering in Minnesota, <br />Wisconsin, and Iowa, but water supply conditions <br />improved substantially during the summer, The <br />southeast, centering in Virginia, the Clp'Oiinas, and <br />Georgia, experienced severe drought conditions later <br />in the summer and in the early fall, While these states <br />were not in the geographical area on which this study <br />coneentrated, their drought conditions fostered na- <br />tionwide participation in the project. <br /> <br />Below normal precipitation amounts continued in <br />the mountain areas critical to water supply through <br />the fall of 1977. By late fall, however, it was obvious <br />that the southwestern desert areas were experiencing <br />above normal precipitation, and significant flooding <br />occurred in Arizona and Southern California, By <br />February, the rains had extended throughout the <br />west, and even the most severely drought impacted <br />communities were dropping water rationing and <br />related measures. As the rainy season ended, it was <br />obvious that many areas would complete the water <br />year with precipitation amounts at or near reeord <br />levels. The drought is now history, but all of those <br />who worked on this project hope that it proves to be a <br />history from which westerners learn many valuable <br />lessons on how to make better use of available water <br />when future shortages occur. <br /> <br />GOVERNMENT RESPONDS <br /> <br />By February 1977, the drought situation was <br />causing sufficient concern throughout the 11 western <br />states to motivate government response, Most <br /> <br />1 <br />