My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WMOD00272
CWCB
>
Weather Modification
>
Backfile
>
WMOD00272
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/28/2009 2:29:16 PM
Creation date
5/16/2007 3:02:42 PM
Metadata
Fields
Template:
Weather Modification
Title
The Feasibility of Operational Cloud Seeding in the North Platte River Basin Headwaters to Increase Mountain Snowfall
Prepared For
US Department of the Interior Bureau of Reclaimation
Prepared By
Jonnie G. Medina, Technical Service Center, Water Resources Services
Date
5/1/2000
County
Statewide
State
CO
Weather Modification - Doc Type
Scientific Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
113
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).
Show annotations
View images
View plain text
<br />4.5.1. Cloud seedability parameter estimated from model simulations <br /> <br />Values in table 4.3 use an enhancement factor of 0.1125 that estimates the percentage increase from <br />cloud seeding. This value is based on the product ofthe two factors, 0.45 and 0.25. The first factor <br />represents the concept that on average, 45 percent of the precipitation (above 9000 feet as used here) in <br />the Headwaters Region is seedable. The 0.25 factor represents that the expected average increase in <br />treated clouds is about 25 percent. The 25 percent increase value is obtained from consideration of the <br />results of the Bridger Range Experiment (Super, 1974; Super and Heimbach, Jr., 1983) and the Climax I <br />and II Experiments (Mielke et aI., 1971; 1981). <br /> <br />The 0.45 factor was calculated as the average of 7 ratios of precipitation obtained from simulations by <br />Colorado State University with the RAMS model, on 7 storms of the 1998-99 winter in the Park Range. <br />The precipitation ratios were defined as total precipitation (using hourly reading from the model) with <br />model liquid water present to total storm precipitation. The storm seedability ratios do not consider <br />information when seeding leads to precipitation when naturally none would occur. The ratio was <br />considered of storm time with liquid water present to total storm time but values appeared unrealistically <br />large and the more conservative ratio was selected. The model did indicate for some periods, lower or no <br />liquid water amounts when model precipitation rate was relatively high. Storms simulated were selected <br />for varying storm types according to time of winter; small, moderate and high actual precipitation <br />amounts, and predominant westerly and nonwesterly wind cases. Three storms were simulated at 3 <br />kilometer grid point resolution and the remainder at 12 kilometer grid spacing. Model simulations <br />appeared to overestimate precipitation (suitable comparisons could not be made because point estimates <br />at field gauge locations were not made by the model). Simulations need to be compared with actual field <br />observations. Generally, the 3 kilometer simulations yield substantial detail for comparisons. The <br />simulations appear to yield useful information for purposes of the proposed program and it is <br />recommended that additional modeling be pursued should the program move forward. <br /> <br />Table 4.1 gives operational project cost information. The average annual cost of operation per seeding <br />device is estimated at $21,301. If water is valued at $30 per ac-ft, the benefit/cost is 2.18 for the 40- <br />percent areal coverage case and 3.28 for 60-percent coverage. It is likely that a generator installation <br />design can be developed that can achieve 40 percent or better areal coverage. <br /> <br />29 <br />
The URL can be used to link to this page
Your browser does not support the video tag.