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<br />~olorado Water Resources Research ln~titute. <br /> <br />mountains, and other areas with more reliable precipi- <br />tation, accumulated deficits only reach about 1.2 years <br />of average precipitation. For example. if Breckenridge <br />averages 22 inches of precipitation per year, a very <br />severe multi.year drought might result in an accumu- <br />lated deficit of more than 22 inches over a few years <br />time before above average precipitation reduces those <br />deficits. <br /> <br />1a:UnJ<Ed~Wi1 <br />IlJ3g> 00 <br /> <br />4)... <br /> <br /> <br />" <br /> <br />'" <br /> <br />< <br /> <br />.< <br /> <br />'" <br /> <br />'" <br /> <br />4> <br /> <br />'" <br /> <br />... <br /> <br />7) Timing of drought - When does it start? When does <br />it end? <br /> <br />Short duration droughts can begin and end in any <br />season. <br /> <br />Major droughts with durations of one year or longer <br />tend to begin in and end in the season that is locally <br />the wet season. This varies from place to place in the <br />state. For example: <br /> <br />Major droughts in the mountains tend to begin or end <br />during the winter or spring months. In extreme <br />southwestern Colorado, significant droughts have <br />both begun and ended in the fall. The more dramatic <br />the seasonal precipitation cycle is, the more difficult <br />it is to end a major drought during the time of year <br />that is the climatological dry season for that area. <br />For example. over eastern Colorado, rhe months of <br />December, January and February are typically dry. <br />The three months combined produce, on average, less <br />than 10% of the annual precipitation. Rarely does <br />enough precipitation fall during this time of year to <br />significantly alleviate longer-term moisture deficits. <br />However, a week or two a/very wet weather during <br />late spring east of the mountains can bring a major <br />drought to an end. For example, the spring of 1995 <br />and the last few days of April 1999 delivered enough <br />precipitation to compensate for large deficits. <br /> <br />There are several extUhples of droughts ending abruptly <br />with the appearance of widespread excess precipitation. <br />For example, the severe drought of the I 950s was <br />followed by the wettest year in Colorado's history in <br />1957. There are other examples of droughts that have <br />ended more subtly, however. <br /> <br />8) Does a dry winter foretell a wet summer? <br /> <br />There is endless folklore concerning drought. Even before <br />"El Nino" found its way into climatological jargon, people <br />have talked ways to predict drought. Does the climate of <br />one season foretell the next? Much folklore would suggest <br />that. Our analyses. howevet, did not bear that out. We <br />looked at a number of combinations. What happens after a <br />very dry winter in the mountains? What happens after a <br />very dry autumn at lower elevations (such as fall 1999 in <br />Colorado)? Our analyses showed that sometimes dry <br />winters in the mountains were followed by wet summers (like <br />1999), but other years they weren't. Sometimes dry springs <br />along the Front Range were folJawed by hot dry summers <br />(like 1954), but other years they weren't. Further analysis <br />wO'uld be required to determine how and if precipitation <br />during one seasO'n helps foretell the next here in ColoradO'. <br />Less than 10% of the variance in summer precipitation is <br />explained anywhere in Colorado by the variations in winter <br />precipitation. <br /> <br />9) Are there drought cycles? <br /> <br />People don't ask climatologists whether there are drought <br />cycles in CO'lorado; most people are positive that there are. <br />Some say there is a 3 year cycle, while others claim 7. The <br />sunspot cycle of II years has caught some people's <br />attention, while many strongly believe that a 22 year <br />drought cycle (double sunspot cycle) controls Colorado's <br />drought patterns. <br /> <br />We examined our rainfall records in ColoradO' in search of <br />drought cycles. There is some evidence af a twO' to' three <br />year cycle over portions of southern and eastern Colorado. <br />The dry periods in the I 890s. 1930s, 1950s and again in the <br />1970s have convinced some observers that the double <br />sunspot cycle really does affect drought patterns in <br />Colorado. That theory doesn't explain why the 19105 were <br />so wet, why parts of the 1960s were very dry, and why we <br />have been wet for the better part of 18 years in a row, but <br />many still believe it. As far a seven or eleven-year cycle, <br />there isn't much supparting evidence for that. It is true that <br />dry periods are foIlowed by wet, and wet followed by dry? <br />That makes a cycle. doesn't it? The problem is that those <br />cycles just aren't very reli.ble. As such, they don't help us <br />much if at all in predicting what will happen next year or the <br />year after that. Even throwing in the irregular cycle of the El <br />Nino Southern Oscillation, we are stin left with a great deal <br />of unexplained variability in our precipitation. <br /> <br />17 <br />