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Current Meteorological Theory of the Condensational Growth of a Stationary Drop
The purpose of this report is to elaborate a specific theory of drop growth by condensation for use in cloud physics and various laboratory calculations related to cloud physics. It has been assimilated, for the most part, from existing literature, but in no one place has it received full exposition...
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creator | Carstens.,John C |
description | The purpose of this report is to elaborate a specific theory of drop growth by condensation for use in cloud physics and various laboratory calculations related to cloud physics. It has been assimilated, for the most part, from existing literature, but in no one place has it received full exposition. This work therefore claims neither comprehensiveness, in treating all aspects and theories of drop growth, nor profundity in revealing new facets of the phenomena. (Author) |
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It has been assimilated, for the most part, from existing literature, but in no one place has it received full exposition. This work therefore claims neither comprehensiveness, in treating all aspects and theories of drop growth, nor profundity in revealing new facets of the phenomena. (Author)</description><language>eng</language><subject>AEROSOLS ; CLOUD PHYSICS ; CLOUDS ; CONDENSATION ; DIFFUSION ; DROPS ; MATHEMATICAL MODELS ; Meteorology</subject><creationdate>1973</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>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,776,881,27544,27545</link.rule.ids><linktorsrc>$$Uhttps://apps.dtic.mil/sti/citations/AD0764258$$EView_record_in_DTIC$$FView_record_in_$$GDTIC$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Carstens.,John C</creatorcontrib><creatorcontrib>MISSOURI UNIV ROLLA DEPT OF PHYSICS</creatorcontrib><title>Current Meteorological Theory of the Condensational Growth of a Stationary Drop</title><description>The purpose of this report is to elaborate a specific theory of drop growth by condensation for use in cloud physics and various laboratory calculations related to cloud physics. 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(Author)</description><subject>AEROSOLS</subject><subject>CLOUD PHYSICS</subject><subject>CLOUDS</subject><subject>CONDENSATION</subject><subject>DIFFUSION</subject><subject>DROPS</subject><subject>MATHEMATICAL MODELS</subject><subject>Meteorology</subject><fulltext>true</fulltext><rsrctype>report</rsrctype><creationdate>1973</creationdate><recordtype>report</recordtype><sourceid>1RU</sourceid><recordid>eNrjZPB3Li0qSs0rUfBNLUnNL8rPyU_PTE7MUQjJAPIqFfLTFEoyUhWc8_NSUvOKE0sy8_OAku5F-eUlGSDJRIXgEogoULFLUX4BDwNrWmJOcSovlOZmkHFzDXH20E0pyUyOLy7JzEstiXd0MTA3MzEytTAmIA0AL-oz4A</recordid><startdate>1973</startdate><enddate>1973</enddate><creator>Carstens.,John C</creator><scope>1RU</scope><scope>BHM</scope></search><sort><creationdate>1973</creationdate><title>Current Meteorological Theory of the Condensational Growth of a Stationary Drop</title><author>Carstens.,John C</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-dtic_stinet_AD07642583</frbrgroupid><rsrctype>reports</rsrctype><prefilter>reports</prefilter><language>eng</language><creationdate>1973</creationdate><topic>AEROSOLS</topic><topic>CLOUD PHYSICS</topic><topic>CLOUDS</topic><topic>CONDENSATION</topic><topic>DIFFUSION</topic><topic>DROPS</topic><topic>MATHEMATICAL MODELS</topic><topic>Meteorology</topic><toplevel>online_resources</toplevel><creatorcontrib>Carstens.,John C</creatorcontrib><creatorcontrib>MISSOURI UNIV ROLLA DEPT OF PHYSICS</creatorcontrib><collection>DTIC Technical Reports</collection><collection>DTIC STINET</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Carstens.,John C</au><aucorp>MISSOURI UNIV ROLLA DEPT OF PHYSICS</aucorp><format>book</format><genre>unknown</genre><ristype>RPRT</ristype><btitle>Current Meteorological Theory of the Condensational Growth of a Stationary Drop</btitle><date>1973</date><risdate>1973</risdate><abstract>The purpose of this report is to elaborate a specific theory of drop growth by condensation for use in cloud physics and various laboratory calculations related to cloud physics. 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language | eng |
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source | DTIC Technical Reports |
subjects | AEROSOLS CLOUD PHYSICS CLOUDS CONDENSATION DIFFUSION DROPS MATHEMATICAL MODELS Meteorology |
title | Current Meteorological Theory of the Condensational Growth of a Stationary Drop |
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