My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WMOD00276
CWCB
>
Weather Modification
>
DayForward
>
WMOD00276
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/28/2009 2:32:19 PM
Creation date
4/11/2008 3:38:39 PM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
85-5071
Title
Cooperative Weather Modification Research Program - 1985 Field Operations Plan
Date
1/1/1985
State
UT
Weather Modification - Doc Type
Report
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
88
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 />. <br /> <br />6. Cloud physics and kinematics experiments. <br />A major objective of the 1985 field research program is to describe <br />the spatial and temporal distribution of supercooled liquid water in the <br />clouds over and near the Tw;har Mtns, the physical processes responsible <br />for precipitation development in the clouds, and the trajectories taken <br />by cloud and precipitation particles. <br />The cloud physics and kinematics investigations required to reach <br />this objective will involve the analysis and interpretation of a variety <br />of data. Most of the data will be collected with remote sensing instru- <br />mentation. The NCAR CP3 C.band Doppler radar will be placed at the base <br />of the Tushar Mtns (elevation 1884 m) (see Figure 1). The WPL Ka-band <br />Doppler dual-polarization radar will be located at a 2568 m elevated <br />"remote sensing" site in Merchant Valley on the slopes of the mountains. <br />The two radars will provid.~ information on .the growth of precipitation <br />particles and on their motions through the clouds. At the remote <br />sensing site there will als.o be the WPL dual-wavelength, steerable <br />microwave radiometer for measurements of liquid water amounts and the UU <br />polarization-diversity ruby- wavelength Iidar for observations of par- <br />ticle phase and shape. (Figure 4 shows the planned. positioning of <br />equipment at the remote sensing site.) I n addition to this array of <br />remote sensing instrumentatnon the AI supercooled liquid water detector <br />(based on the Rosemount aviation icing rate device) will be placed at a <br />high elevation (2975 m) exposed site likely to be in supercooled cloud. <br />Surface observations of p,"ecipitation mass, number and mass flux, <br />crystal habit, state of aggregation, state of riming, etc. will be made <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />-32- <br /> <br />. <br />
The URL can be used to link to this page
Your browser does not support the video tag.