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forward when in fact precipitation in particular was less than expected on a daily or monthly <br /> basis rather than an annual basis. Nevertheless, the effective cumulative precipitation that is <br /> important for plant growth remained high for the rest of the year and for that aspect the annual <br /> graph is quite relevant. <br /> In 2014, the above normal precipitation continued, although February and March were a bit on <br /> the dry side. Temperatures were near normal until May when temperatures tended to be below <br /> normal and that continued well into June. In fact,by July 1 only about 5 days above 90 <br /> degrees occurred at DIA(and elsewhere in the metro area)when normal would be about 12 <br /> days. Summer finally arrived in early July with high temperatures and low precipitation. But <br /> by the time of this report writing that was already changing back to a continued tendency <br /> toward dampness and somewhat below normal or normal temperatures. <br /> It is common for the Denver area to experience pronounced drying in June and usually a heat <br /> wave of some degree from mid-June to about mid-July. So far, that normal pattern appears to <br /> have been reduced to only a week or two in 2014. Furthermore,with a moderate El Nino <br /> developing this increased moisture and reduced heat may continue through the rest of the year. <br /> Long term predictions are trending in that direction,but things can change quickly. One of the <br /> big puzzles in climatology is how these long term cycles like ENSO will behave in a changing <br /> world climate. Will they just behave normally and global climate change simply be a modifier <br /> or will global climate change alter the behavior of the cycles? At this point there are only <br /> theories,hypotheses and suppositions,but some interaction will undoubtedly occur. What <br /> those interactions will result in is the mystery. <br /> In conclusion, the weather and climate patterns since about September 10, 2013, to the present <br /> have certainly been favorable for vegetation growth and recovery from years and years of sub- <br /> optimal to disastrous drought conditions. In fact, to this observer,the vegetation at the Lowry <br /> Range is the best ever seen in nearly 20 years of regularly visiting the site. That applies to both <br /> the natural vegetation,but also the reclamation areas, and, unfortunately,the weeds as well. <br /> The better conditions favors all, including undesirable weed species,however this observer's <br /> 50+years of experience with the development patterns of vegetation on drastically disturbed <br /> land as well as the recovery on land with less disturbance than total disruption,the native <br /> vegetation at this site is not only holding its own in the competitive struggles with aggressive <br /> weeds but is actually improving in spite of the weeds. Wet and cool years like late 2013 and <br /> the first half of 2014 certainly has played a very large role in this development, but other <br /> factors also are of significance. Favorable growing conditions have certainly made it easier, <br /> but one must be careful to not place to much praise on climatic conditions. It is not the whole <br /> story. Drought years, ironically, have also contributed to this fine recovery. <br /> 2. Topsoiling-Topsoil was spread on approximately 32 acres for reclamation. <br /> A. Locations of topsoiling- Topsoiling occurred on the land on the south end of the <br /> older mining areas and on the west side of the main road. <br /> Status report for 2014 due July 15, 2014 Page 6 of 10 <br />