Laserfiche WebLink
<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />i I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />The area of the Pawnee Creek watershed is very sparsely populated. However, a <br />remarkably large percentage of the residents of this ranching and dryland fanning area <br />were equipped with rain gauges and attempted to measure the rainfall. This evaluation of <br />the original rainfall reports gathered after the storm found that most reports and . <br />observations in the areas of heaviest rainfall were estimates as opposed to accurate gauge <br />measurements since most rain gauges overflowed. Some of these estimates were derived <br />from stock tank levels and water depths in 5-gallon buckets. A few rainfall reports near <br />the storm center likely included rain from previous days or from splash from surface <br />water, thus placing in question some of the largest reports. Nevertheless, there was <br />convincing evidence that rainfall totals for the evening of July 29 into the early morning of <br />July 30, 1997 exceeded 12 inches and locally approached 14 inches over an area of <br />perhaps 17 square miles. <br /> <br />The 1998 survey uncovered several more observations that apparently were not obtained <br />for the original analysis. These additional data suggest that the original survey may have <br />underestimated rainfall in some areas, particularly over eastern Weld County. A re- <br />analysis shows that rainfall totals for the evening may have exceeded six inches over on <br />area of approximately 270 square miles. The areas of greatest uncertainty in this analysis <br />include portions of western Logan county just east of the storm's center and a narrow <br />band extending southwestward to just northwest of New Raymer where there are solid <br />indications of extreme rainfall but few confident observations. <br /> <br />In addition to ground measurements of rainfall, the National Weather Service radar data <br />were collected and are available to help estimate storm rainfall for areas without gauge <br />measurements, These radar data proved very helpful in defining storm locations, duration, <br />and areas of maximum rainfall over Morgan and Weld counties, but were less helpful over <br />Logan County which is farther away from the radar transceiver. <br /> <br />In conclusion, despite the low population density of the area, a reasonably confident <br />depiction of storm rainfall has been assembled suitable for hydrologic and engineering <br />applications. The Pawnee Creek storm of July 29-30, 1997 was, indeed, an extreme event <br />in terms of total rainfall depth, area and duration. It will stand out for many years to come <br />as one of just a handful of extreme rainfall events in eastern Colorado's recorded history <br />with rainfall totals exceeding 12 inches in a duration ofless than 12 hours. <br /> <br />III <br />