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<br />I <br /> <br />I <br /> <br />Figure 41 shows the backing of the 10,000 ft. wind at Mt. Harris re- <br />lative to the more northerly macroscale observations. This effect is obser- <br />ved quite consistently under 3100_3600 flow conditions and is believed to be <br />organized lee troughing over the Yampa Valley in the lee of the Elkhead Mou- <br />ntains which lie at a mean elevation of around 9600 feet, twenty miles north <br />of the balloon release site. Figure 42 is a topography cross- section for 330': <br />3400 azimuth from Steamboat Springs to the Montana-Wyoming border. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />HYDROLOGICAL DAT A <br /> <br />I <br /> <br />Soil Conservation Service personnel took snowcourse readings through- <br />out the 1965-66wiliJ.ter season." The valley thaw began March 15, 1966, <br />and the ridge thaw about April 6, 1966; values beyond these dates are not <br />used for analysis purposes. <br /> <br />I <br /> <br />I <br /> <br />The original data will be analyzed by the Soil Conservation Service <br />in a separate report to the Bureau of Reclamation. In our analysis work, we <br />fir st normalized each set of data points to the water content value at Buffalo <br />Pass; tabular results of this computation are shown in Table VI. The data <br /> <br />I <br /> <br />I <br /> <br />were next plotted as a function of station location, as shown in Figure 43 to <br />dete rmine their relative value s with re spect to similar data analyzed during <br />Phase I. We then computed the mean for the 1965-66 season and the error <br />of the mean; the 1964-65 mean and 1965-66 mean, as well as the average <br />error of the means for those two seasons, are listed in Table VII. Neglect- <br />ing the valley stations- -which this year experienc ed inte rmittent thawing-- <br />the only significant changes are seen to be at Columbine and Rabbit Ears <br />Pass. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Rabbit Ears Pass is on the summit of the Park Range at the south ex- <br />tremity of the target area. Columbine is only about two mile s line-of- sight <br />from Rabbit Ears but is on the leeward side of the ridge. This year! s data <br />indicate a significant change in Rabbit Ears Pass in the plus direction and a <br />significant change at Columbine in the negative direction. It is not possible <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />- 68 - I <br />