Extinction by Aerosol Clouds of Nonspherical Particles at Arbitrary Wavelengths

Extinction by a cloud consisting of many aerosol particles has been found to fall into two distinct wavelength regions which are adequately described by the geometric optics theory and the Rayleigh theory. Because the cloud consists of many different particles, the narrow extinction resonance struct...

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description Extinction by a cloud consisting of many aerosol particles has been found to fall into two distinct wavelength regions which are adequately described by the geometric optics theory and the Rayleigh theory. Because the cloud consists of many different particles, the narrow extinction resonance structure of individual particles is lost, and extinction is governed by shape and size as predicted by geometric optics. At longer wavelengths, particles are in the Rayleigh region, and extinction for a large variety of particle shapes is predicted by the Rayleigh ellipsoidal theory. The transition region lying between the applicability of these two simple theories occupies only about one wavelength decade.
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Because the cloud consists of many different particles, the narrow extinction resonance structure of individual particles is lost, and extinction is governed by shape and size as predicted by geometric optics. At longer wavelengths, particles are in the Rayleigh region, and extinction for a large variety of particle shapes is predicted by the Rayleigh ellipsoidal theory. The transition region lying between the applicability of these two simple theories occupies only about one wavelength decade.</description><language>eng</language><subject>Aerosols ; AS554 ; Clouds ; Ellipsoids ; Extinction ; Geometry ; Optics ; Particles ; PE62622A ; Rayleigh scattering ; Refractive index ; Wavelength</subject><creationdate>1982</creationdate><rights>APPROVED FOR PUBLIC RELEASE</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,780,885,27567,27568</link.rule.ids><linktorsrc>$$Uhttps://apps.dtic.mil/sti/citations/ADA113535$$EView_record_in_DTIC$$FView_record_in_$$GDTIC$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Embury,Janon F</creatorcontrib><creatorcontrib>ARMY ARMAMENT RESEARCH AND DEVELOPMENT COMMAND ABERDEEN PROVING GROUND MD CHEMICAL SYSTEMS LAB</creatorcontrib><title>Extinction by Aerosol Clouds of Nonspherical Particles at Arbitrary Wavelengths</title><description>Extinction by a cloud consisting of many aerosol particles has been found to fall into two distinct wavelength regions which are adequately described by the geometric optics theory and the Rayleigh theory. 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The transition region lying between the applicability of these two simple theories occupies only about one wavelength decade.</description><subject>Aerosols</subject><subject>AS554</subject><subject>Clouds</subject><subject>Ellipsoids</subject><subject>Extinction</subject><subject>Geometry</subject><subject>Optics</subject><subject>Particles</subject><subject>PE62622A</subject><subject>Rayleigh scattering</subject><subject>Refractive index</subject><subject>Wavelength</subject><fulltext>true</fulltext><rsrctype>report</rsrctype><creationdate>1982</creationdate><recordtype>report</recordtype><sourceid>1RU</sourceid><recordid>eNrjZPB3rSjJzEsuyczPU0iqVHBMLcovzs9RcM7JL00pVshPU_DLzysuyEgtykxOzFEISCwqyUzOSS1WSCxRcCxKyiwpSiyqVAhPLEvNSc1LL8ko5mFgTUvMKU7lhdLcDDJuriHOHropQI3xxUC7UkviHV0cDQ2NTYGQgDQAOTM0JA</recordid><startdate>198203</startdate><enddate>198203</enddate><creator>Embury,Janon F</creator><scope>1RU</scope><scope>BHM</scope></search><sort><creationdate>198203</creationdate><title>Extinction by Aerosol Clouds of Nonspherical Particles at Arbitrary Wavelengths</title><author>Embury,Janon F</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-dtic_stinet_ADA1135353</frbrgroupid><rsrctype>reports</rsrctype><prefilter>reports</prefilter><language>eng</language><creationdate>1982</creationdate><topic>Aerosols</topic><topic>AS554</topic><topic>Clouds</topic><topic>Ellipsoids</topic><topic>Extinction</topic><topic>Geometry</topic><topic>Optics</topic><topic>Particles</topic><topic>PE62622A</topic><topic>Rayleigh scattering</topic><topic>Refractive index</topic><topic>Wavelength</topic><toplevel>online_resources</toplevel><creatorcontrib>Embury,Janon F</creatorcontrib><creatorcontrib>ARMY ARMAMENT RESEARCH AND DEVELOPMENT COMMAND ABERDEEN PROVING GROUND MD CHEMICAL SYSTEMS LAB</creatorcontrib><collection>DTIC Technical Reports</collection><collection>DTIC STINET</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Embury,Janon F</au><aucorp>ARMY ARMAMENT RESEARCH AND DEVELOPMENT COMMAND ABERDEEN PROVING GROUND MD CHEMICAL SYSTEMS LAB</aucorp><format>book</format><genre>unknown</genre><ristype>RPRT</ristype><btitle>Extinction by Aerosol Clouds of Nonspherical Particles at Arbitrary Wavelengths</btitle><date>1982-03</date><risdate>1982</risdate><abstract>Extinction by a cloud consisting of many aerosol particles has been found to fall into two distinct wavelength regions which are adequately described by the geometric optics theory and the Rayleigh theory. Because the cloud consists of many different particles, the narrow extinction resonance structure of individual particles is lost, and extinction is governed by shape and size as predicted by geometric optics. At longer wavelengths, particles are in the Rayleigh region, and extinction for a large variety of particle shapes is predicted by the Rayleigh ellipsoidal theory. The transition region lying between the applicability of these two simple theories occupies only about one wavelength decade.</abstract><oa>free_for_read</oa></addata></record>
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source DTIC Technical Reports
subjects Aerosols
AS554
Clouds
Ellipsoids
Extinction
Geometry
Optics
Particles
PE62622A
Rayleigh scattering
Refractive index
Wavelength
title Extinction by Aerosol Clouds of Nonspherical Particles at Arbitrary Wavelengths
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