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<br />Historical Perspectives on Colorado Drought <br /> <br /> <br />. <br /> <br />l <br /> <br />Stream Aow Based on Tree Rtng Evidence, <br />Boulder Creek Near Ck-odell <br /> <br />PToj.et.dflow'or2002 <br />(.dJust.dtob.const$t~WIIh <br />truring dlQ).32.ooo AF <br /> <br />L_st.,..... b...d 01'1 trH <br />ring fYkMnc. .29.600 A; . <br />. ""'" <br />FIow.1J.700AF <br /> <br />1.0.... <br /> <br />110,'" <br /> <br />Tree ring <br />analysis of <br />streamflow <br />suggests that <br />the 2002 <br />drought is the <br />severest to <br />impact <br />northeastern <br />Colorado In <br />almost 300 <br />years! <br /> <br /> <br />140.... <br /> <br />120,000 <br /> <br />100,00' <br /> <br />80,0" <br /> <br />10,1'0 <br /> <br />40,000 <br /> <br />20,000 <br /> <br />. <br />11'0 <br /> <br />2000 <br /> <br />1115 <br /> <br />Figure 3 Streamflow on Boulder Creek based on tree ring analysis near Ordel <br />Colorado that shows the comparative impact of droughts since 1700. <br /> <br />Creek <br /> <br />Press <br /> <br />More than half the state has been in moderate drought during the droughts of the <br />1890's. 1930's and the current drought of 1999-2003. However. short-term droughts <br />(3.momh duration) have previously covered as much as 80% of the slate, and longer- <br />duration droughts (2-4 years) have encompassed as much as 70% of the state. <br /> <br /> <br />The data in Table 2., edited from a table <br />in r-.1cKee et al. (2000), "shows the <br />periods during which at least 60% of <br />Colorado was dr)\ as determined by <br />the Standardiled Precipitation Index <br />(Sill) values for 2-4-month periods:' <br />Notc that the dates are not identical to <br />those discussed above, as they were <br />determined using a different <br />methodology, namely the SPI instead of <br />water year precipitation totals. Ilowever, it is clear that the 1999.2002 drought ranks <br />as one of the most severe to affect the state during the instrumented period ofn..'Cord <br />The questiun remains how this drought compares to historical droughts of the past <br />300 to 500 years. Paleo-climalology may prO\:ide that insight. <br /> <br />ears <br />cars <br />cars <br /> <br />cars <br />cars <br /> <br />Page 6 <br /> <br />paper <br /> <br />HDR Engineering. Inc. <br />Printed 00 30% posl-coosumer recycled content <br /> <br /> <br />~ <br />. <br />~ <br />~ <br />" <br />c <br />.; <br />~ <br />;; <br />> <br />. <br />. <br />~ <br />" <br />.. <br />. <br />:> <br />.. <br />. <br />" <br />" <br />c <br /> <br />115. <br /> <br />1125 <br /> <br />t'OO <br /> <br />tin <br /> <br />tl5. <br /> <br />tl25 <br /> <br />tlOO <br /> <br />t175 <br /> <br />1750 <br /> <br />t725 <br /> <br />Hydrosphere qualified the regional significance ufthe study, saying, "Boulder <br />is fairly representative of most of the northern Front Range and most of the <br />tributaries into the Colorado.Big Thompson (system] as well" (Associated <br />2002). <br /> <br />2 <br />o <br />6 <br />4' <br />~ <br />2 <br />3 <br /> <br />905 <br />-l9-l1 <br />\-\957 <br />999-2002 <br />-- <br />963- 965 <br />-- <br />975 978 <br /> <br />-\ <br /> <br />893- <br />93 <br />95 <br />