My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WMOD00514
CWCB
>
Weather Modification
>
DayForward
>
WMOD00514
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/28/2009 2:40:29 PM
Creation date
4/24/2008 2:51:14 PM
Metadata
Fields
Template:
Weather Modification
Title
Preliminary Field Experiments of Snowmax on Cumulus Mediocris Clouds to Artificially Induce the Production of Ice Particles
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.
/
5
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 />'r <br /> <br />:--i<-<' <br /> <br />Preliminary Field Experiments of Snomax™ on Cumulus Mediocris Clouds~ <br />Artificially Induce the Production of Ice Particles. <br /> <br />James A. Jung in conjunction with <br />North Dakota Atmospheric Resource Board <br />P. O. Box 1833 <br />Bismarck, NO 58502 <br /> <br />Snomax Technologies <br />95 AlIens Creek Rd. <br />Rochester, NY 14618 <br /> <br />ABSTRACT <br /> <br />SnomaxTH Snow Inducer, Pseudomonas syringae, has undergone preliminary <br />field studies to determine its ability to produce ice particles in <br />cumulus type clouds. Initial results show the production of ice <br />particles at concentrations of 100's/liter within 8 miputes after <br />seeding with SnomaxTH at temperatures near -5oC. <br /> <br />1. Introduction <br /> <br />The presence or absence of ice par- <br />ticles in continental cumulus clouds gen- <br />erally determines its efficiency to <br />produce rain on the ground. Typically, <br />except for the low concentrations of <br />biogenic ice nuclei (Schnell and Vali, <br />1976; Levin and Yankosky, 1988; Vali et <br />al., 1976) the atmosphere has a very <br />limited supply of active ice nuclei at <br />temperatures warmer than --150C. Even at <br />-200C the average number of effective ice <br />nuclei in the atmosphere is only about 1 <br />liter-1 (Pruppacher and Klett, 1980). <br />Consequently this deficiency of effective <br />ice nuclei in continental c0Gvective <br />clouds, with cloud top temperatures <br />greater than about -12oC, produce little <br />or no rain (Pruppacher and Klett 1980). <br />It is known that large numbers of <br />living and dead microorganisms can be <br />found in rain, hail and ~;now (Gregory, <br />1967; Parker, 1968; Parker and Barso] m, <br />1970: Mandrioli et aI., 1973). Thc'se <br />microorganisms were assumed to be swept <br />out or collected by falling hydrometeors <br />until Schnell and Vali (1972, 1973) re- <br />ported that some of these microorganisms <br />were actually used as freezing nuclei. <br />Vali et aI. (1976) isolated a bac- <br />terial culture from decomposing leaves <br />which was the most effective in producing <br />freezing nuclei. Maki et al., (1974) <br />identified the bacteria as Pseudomonas <br />syringae, a bacteria normally found on <br />plant surfaces as an epiphyte. This ice <br />nucleation-active bacteria was found to be <br />active at temperatures between -20 and <br />-100C (Maki and Willoughby, 1978: Lindow <br />et aI.. 1978: Yankofsky et aI., 1981b: <br />Lindowet al.. 1982). Figure 1 compares <br />the bacterial freezing spectrum of Snomax <br />to AgI and dry ice. AgI activates between <br />-80 and -12cC, while Snomax will initiate <br />the the formation of ice at significantly <br />wa rmer ten:peratures (Ward and DeMo'tt <br />1989) . <br />Snomax (Pseudomonas syringae) aerosols <br />were found to be highly efficient and fast <br />acting, apparently nucleating ice by a <br /> <br />IOf~ <br /> <br />J(.-_x <br />-..... <br />, <br /> <br />~ <br />\ <br />I <br />I <br />. <br /> <br />o Snomdx <br /> <br />10'. <br /> <br />x Ag I (SOL' f'/ J <br />o ^9I (PYROI <br />A Dry Ice <br /> <br />.~ <br />~ 10" <br />o <br />t;:i IOIZ <br />;: <br /> <br />lOll <br /> <br />'0" <br />... <br /> <br />-12 .6 -4 <br />TEMP(RATURE (.C) <br /> <br />o <br /> <br />F<.guJte. 1. CompaJU.6 on 06 .the. ice. CJuj.6.ta..t <br />yie.ld ve.M w.. .te.mpe.JLa.t.Wte. nOJt Snomax., MY <br />ice., and two 06 .the. mOJte. e.66icie.n.t AgI- <br />.type. ice. nucte.a..t<.ng ae.JtO.60t6 nlWm .6o.tu- <br />lion c.ombw..lion and PYIW.te.chrUc .60Junut- <br />a..t<.on. (6Jtom Wand and Ve.Mo.t..t., 1999) <br /> <br />condensation freezing mechanism and at <br />rates comparable to those of dry ice (Ward <br />and DeMott. 1988). Preliminary field <br />tests with Snomax showed visible <br />glaciation effects at temperatures as warm <br />as -50C (Ward and DeMott, 1988). These <br />results suggest a great potential for <br />Snomax as another ice nUCleating agent for <br />use in weather modification. <br />This paper reports some initial <br />results of seeding cumulus clouds with <br />Snomax for the purpose of ice production <br />for weather modification purposes. <br /> <br />2. PROCEDURE <br /> <br />2.1 Seeding Hypothesis <br /> <br />To study the effects of Snomax as a <br />cloud-ice initiating agent, cumulus type <br />clouds were used. These cumulus had cloud <br />top temperatures warmer than -6oC and had <br />little or no natural ,ceo These clouds <br />were seeded with a mixture of 80% <br />Pseudomonas syringae and 20% silica base <br />at the rate of 20 g min-1 during the <br />entire time the aircraft was in-cloud. <br />After seeding, subsequent penetrations <br />were made through the cloud near the same <br />height to measure the number of ice part- <br />icles. The liquid water content of the <br />cloud was also to be measured, but a <br /> <br />153 <br />
The URL can be used to link to this page
Your browser does not support the video tag.