My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WSPC06829
CWCB
>
Water Supply Protection
>
Backfile
>
19000-19999
>
WSPC06829
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 12:08:00 PM
Creation date
10/9/2006 6:05:56 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8200.700
Description
Colorado River Basin General Publications - Augmentation-Weather Modification
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
4/15/1983
Author
DOI-BOR
Title
CREST - Colorado River Enhanced Snowpack Test - Program Plan
Water Supply Pro - Doc Type
Report/Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
55
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 />000176 <br /> <br />changes which occur in the clouds and on the ground. Fully instru- <br />mented cloud physics aircraft will be required, as will surface <br />monitors such as radars, microwave radiometers, icing rate meters, <br />snowfall rate sensors, and other specialized equipment. Mobile <br />facilities will be transported throughout the subbasins to conduct this <br />work. <br /> <br />C. Extra-Area Effects <br /> <br />The need to address the possible existence of effects beyond the target area <br />and their consequences is explicitly recognized as an important component <br />of the CREST Program. <br /> <br />The major extra-area effects issue concerns whether seeding increases or <br />decreases snowfall in the regions immediately downwind of the areas <br />targeted for precipitation augmentation. The region of concern encompasses <br />the lee slope of the mountain ranges targeted for cloud seeding and the <br />crests of the next major ranges downwind. If effects cannot be found <br />there, a search for them at a greater distance is likely to be fruitless. <br /> <br />A second important issue is whether the seeding may affect the development <br />of storm systems as they pass beyond the targets and move into the lee of <br />the Rockies, a region well known to meteorologists as the birthplace of <br />new storms and a place where weak storms are likely to find new strength. <br />If seeding were to affect the subsequent history of the storm, the results <br />would be of significant importance for any program of precipitation <br />management. The likelihood, though considered small, cannot be dismissed. <br /> <br />Any effect that cloud seeding has on precipitation and storm development <br />beyond the target area will affect the natural environment and, more <br />immediately, the activities of people in the region thus influenced. <br /> <br />The study of these impacts will continue to be addressed along with <br />environmental requirements for acceptable precipitation management. The <br />specific role of the extra-area effects program element for CREST will be <br />to supply the basic data regarding precipitation in the downwind areas of <br />the CREST targets. <br /> <br />Snow gages, like those used in the primary target areas, will be placed on <br />the lee slopes of the target ranges and in the heavy snowbelts of immedi- <br />ate downwind ranges. Density of placement will be reduced to about one- <br />fifth that in the primary targets. Initially, maximum use will be made of <br />ski areas and other manned high-altitude locations as gage sites. Later, <br />remote gages will be installed to complete the network. Observations from <br />these gages will become part of the project data bank, available for <br />analysis capable of detecting precipitation changes comparable to those <br />analyzed in the primary target areas. In addition, analyses will be <br />conducted to see if precipitation that could be associated with seeding in <br />the target area can be identified through the presence of seeding agents <br />in the snow. <br /> <br />The farther away one looks for possible effects of cloud seeding, the <br />more the direct effect of the seeding becomes confused with strengthening, <br />weakening, or other changes in the structure of the storm itself. <br /> <br />35 <br />
The URL can be used to link to this page
Your browser does not support the video tag.