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2025-06-30_PERMIT FILE - C1981019
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2025-06-30_PERMIT FILE - C1981019
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Last modified
6/30/2025 10:26:45 AM
Creation date
6/30/2025 10:09:30 AM
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Template:
DRMS Permit Index
Permit No
C1981019
IBM Index Class Name
Permit File
Doc Date
6/30/2025
Section_Exhibit Name
2.04 Information on Environmental Resources
Media Type
D
Archive
No
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RULE 2 PERMITS <br /> <br />Rule 2 Permits 2.04-42 Revision Date: 11/1/21 <br /> Revision No.: TR-150 <br />Precipitation <br /> <br />Precipitation information for Craig and Meeker is shown in Table 2.04.8-1, Monthly Normals of <br />Temperature and Precipitation (1941-1970), in Table 2.04.8-2 Monthly Precipitation (1971-1979) <br />for Craig, Colorado and Table 2.04.8-3, Monthly Precipitation (1971-1979) for Meeker, Colorado. <br /> <br />Temperature <br /> <br />Temperature data for Craig and Meeker are presented in Table 2.04.8-1, Monthly Normals of <br />Temperature and Precipitation (1941-1970), in Table 2.04.8-4, Monthly Average Temperature <br />(1971-1979) for Craig, Colorado and in Table 2.04.8-5, Monthly Average Temperature (1971- <br />1979) for Meeker, Colorado. Based on data collected by the United States Department of <br />Commerce, the mean annual temperature of Craig is 42.4°F while the mean annual temperature at <br />Meeker is 44.2°F. Mean maximum and minimum monthly temperatures for both Craig and Meeker <br />are shown in Table 2.04.8-6, Temperature Summary - Means. <br /> <br />Wind <br /> <br />The synoptic flow in the area is characterized by prevailing westerly winds, which influence air <br />quality in the region. The direction and speed of the winds are greatly affected by the local <br />topography. <br /> <br />The general area contains two large drainage basins: the Yampa River Basin and the Williams <br />Fork River drainage system. The Yampa Valley forms a broad canyon which channels the airflow <br />into an east-west orientation reflecting upslope and downslope motion. Similar upslope- <br />downslope wind flow exists in the Williams Fork Valley. The flow draining this Valley is directed <br />northwardly along the high ground west of Craig prior to joining the main stream flowing up and <br />down the Yampa Valley at the end of the ridge. <br /> <br />The high frequency of near-calm conditions exists because of the protection afforded by the local <br />terrain in most of the valleys. These conditions generally occur at night and in the early morning. <br />The strongest winds in the area can be expected during the winter and early spring, especially in <br />March, and briefly during summer thunderstorms. <br /> <br />The prevailing winds over most of the permit area will be from the southwest at an average speed <br />of approximately 8 to 9 miles per hour; some 10 to 15 percent of the time the wind will blow out <br />of the northeast. Strong winds will occur due to cold fronts and thunderstorms moving through the <br />area, but fair weather winds will rarely exceed 20 to 25 miles per hour. <br /> <br />Meteorological Work at Colowyo <br /> <br />Site specific meteorology and total suspended particulate analyses for the Colowyo operation are <br />set forth in Exhibit 8, Air Quality Information under the title of "Report of Site Meteorology and <br />Total Suspended Particulate Studies." This one year baseline monitoring program was conducted <br />by Western Scientific Services, Inc. of Fort Collins, Colorado during 1976. <br />
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