My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2020-03-24_PERMIT FILE - C1981019A (5)
DRMS
>
Day Forward
>
Permit File
>
Coal
>
C1981019
>
2020-03-24_PERMIT FILE - C1981019A (5)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/4/2020 6:34:06 PM
Creation date
5/11/2020 3:31:32 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981019A
IBM Index Class Name
Permit File
Doc Date
3/24/2020
Type & Sequence
TR135
Section_Exhibit Name
2.04 Information on Environmental Resources
Media Type
D
Archive
Yes
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
69
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
RULE 2 PERMITS <br /> Temperature <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 /> Wind <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 /> 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 /> 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 /> 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 /> Meteorological Work at Colowyo <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 /> Site-specific precipitation data obtained at the Colowyo operation are presented in Table 2.04.8-7, <br /> Monthly Precipitation- Colowyo Permit Area. <br /> Representative wind roses are set forth in Figure 2.04.8-1, Wind Rose — Mine Site and Figure <br /> 2.04.8-2, Wind Rose—Gossard Loadout. <br /> Rule 2 Permits 2.04-42 Revision Date: 12/20/19 <br /> Revision No.: TR-135 <br />
The URL can be used to link to this page
Your browser does not support the video tag.