My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WMOD00551
CWCB
>
Weather Modification
>
DayForward
>
WMOD00551
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/28/2009 2:40:46 PM
Creation date
4/24/2008 2:55:11 PM
Metadata
Fields
Template:
Weather Modification
Title
The South Dakota Weather Modiication Program: Adminitration, Operations and Technology
Date
9/1/1974
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.
/
51
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 />RAIN DROPS -SIZE AND EVAPORATION <br /> <br />Rain drops always evaporate to some extent as they fall from <br />a cloud to the ground. <br /> <br />The amount of evaporation depends on several different factors, <br />some of which are: <br /> <br />, <br /> <br />1. The height of cloud base above the ground. <br /> <br />2. How dry the air is between cloud and the ground. <br /> <br />3. How big the rain drops are which the cloud produces. <br /> <br />All influence how much of the rain will ultimately reach the <br />ground. <br /> <br />Generally rain drops are small. <br /> <br />In an "average" cloud, over 40% of the rain drops are 1/16 <br />inch in diameter and smaller. The largest drclps rarely <br />exceed about 5/32 inch in diameter in any cloud. <br /> <br />The size of the rain drops depends, most strongly, on the <br />cloud's updraft - also, upon the amount of water vapor pre- <br />sent in the air forming these updrafts. <br /> <br />THIN <br /> <br /> <br />1 0, 0 0 0 <br /> <br /> <br />20,000 <br /> <br />15,000 <br /> <br />-'---~/ <br /> <br />~ <br /> <br />YT <br /> <br />33 <br /> <br /> <br />THICK <br />
The URL can be used to link to this page
Your browser does not support the video tag.