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Effective Density Derived from Laboratory Measurements of the Vapor Growth Rates of Small Ice Crystals at −65° to −40°C
An electrodynamic levitation thermal-gradient diffusion chamber was used to grow 268 individual, small ice particles (initial radii of 8–26 μ m) from the vapor, at temperatures ranging from −65° to −40°C, and supersaturations up to liquid saturation. Growth limited by attachment kinetics was frequen...
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Published in: | Journal of the atmospheric sciences 2023-02, Vol.80 (2), p.501-517 |
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creator | Pokrifka, Gwenore F. Moyle, Alfred M. Harrington, Jerry Y. |
description | An electrodynamic levitation thermal-gradient diffusion chamber was used to grow 268 individual, small ice particles (initial radii of 8–26
μ
m) from the vapor, at temperatures ranging from −65° to −40°C, and supersaturations up to liquid saturation. Growth limited by attachment kinetics was frequently measured at low supersaturation, as shown in prior work. At high supersaturation, enhanced growth was measured, likely due to the development of branches and hollowed facets. The effects of branching and hollowing on particle growth are often treated with an effective density
ρ
eff
. We fit the measured time series with two different models to estimate size-dependent
ρ
eff
values: the first model decreases
ρ
eff
to an asymptotic deposition density
ρ
dep
, and the second models
ρ
eff
by a power law with exponent
P
. Both methods produce similar results, though the fits with
ρ
dep
typically have lower relative errors. The fit results do not correspond well with models of isometric or planar single-crystalline growth. While single-crystalline columnar crystals correspond to some of the highest growth rates, a newly constructed geometric model of budding rosette crystals produces the best match with the growth data. The relative frequency of occurrence of
ρ
dep
and
P
values show a clear dependence on ice supersaturation normalized to liquid saturation. We use these relative frequencies of
ρ
dep
and
P
to derive two supersaturation-dependent mass–size relationships suitable for cloud modeling applications. |
doi_str_mv | 10.1175/JAS-D-22-0077.1 |
format | article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2806975450</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2806975450</sourcerecordid><originalsourceid>FETCH-LOGICAL-c240t-62e7cbab706d69798fed3279c57d7ba52ae121e1cfcefa3c3b87f451cb8ec9763</originalsourceid><addsrcrecordid>eNotkM1OAjEUhRujiYiu3TZxPdB2fjqzJAMiBmMi6rbpdG4DhKHYFs0s3Lv2SXgGHsUnsYh3c-7Nd3JuchC6pqRHKU_794NZNIwYiwjhvEdPUIemjEQkyYpT1CEkkKRg-Tm6cG5JwjBOO-hzpDUov3gHPIS1W_g2qA1njbU1DZ7KyljpjW3xA0i3tdDA2jtsNPZzwK9yYyweW_Ph5_hJevgjs0auVniiAJe2dV6uHJYe_3x9Z-l-h705rAnZ78pLdKYDhat_7aKX29FzeRdNH8eTcjCNFEuIjzIGXFWy4iSrs4IXuYY6ZrxQKa95JVMmgTIKVGkFWsYqrnKuk5SqKgdV8Czuoptj7saaty04L5Zma9fhpWA5CZFpkpLg6h9dyhrnLGixsYtG2lZQIg4di9CxGArGxKFjQeNflYxy-A</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2806975450</pqid></control><display><type>article</type><title>Effective Density Derived from Laboratory Measurements of the Vapor Growth Rates of Small Ice Crystals at −65° to −40°C</title><source>EZB Electronic Journals Library</source><creator>Pokrifka, Gwenore F. ; Moyle, Alfred M. ; Harrington, Jerry Y.</creator><creatorcontrib>Pokrifka, Gwenore F. ; Moyle, Alfred M. ; Harrington, Jerry Y.</creatorcontrib><description>An electrodynamic levitation thermal-gradient diffusion chamber was used to grow 268 individual, small ice particles (initial radii of 8–26
μ
m) from the vapor, at temperatures ranging from −65° to −40°C, and supersaturations up to liquid saturation. Growth limited by attachment kinetics was frequently measured at low supersaturation, as shown in prior work. At high supersaturation, enhanced growth was measured, likely due to the development of branches and hollowed facets. The effects of branching and hollowing on particle growth are often treated with an effective density
ρ
eff
. We fit the measured time series with two different models to estimate size-dependent
ρ
eff
values: the first model decreases
ρ
eff
to an asymptotic deposition density
ρ
dep
, and the second models
ρ
eff
by a power law with exponent
P
. Both methods produce similar results, though the fits with
ρ
dep
typically have lower relative errors. The fit results do not correspond well with models of isometric or planar single-crystalline growth. While single-crystalline columnar crystals correspond to some of the highest growth rates, a newly constructed geometric model of budding rosette crystals produces the best match with the growth data. The relative frequency of occurrence of
ρ
dep
and
P
values show a clear dependence on ice supersaturation normalized to liquid saturation. We use these relative frequencies of
ρ
dep
and
P
to derive two supersaturation-dependent mass–size relationships suitable for cloud modeling applications.</description><identifier>ISSN: 0022-4928</identifier><identifier>EISSN: 1520-0469</identifier><identifier>DOI: 10.1175/JAS-D-22-0077.1</identifier><language>eng</language><publisher>Boston: American Meteorological Society</publisher><subject>Aircraft ; Budding ; Crystals ; Density ; Diffusion chambers ; Experiments ; Growth models ; Growth rate ; Ice ; Ice crystals ; Ice particles ; Isometric ; Kinetics ; Laboratories ; Levitation ; Modelling ; Production methods ; Saturation ; Single crystals ; Supersaturation ; Time series ; Vapors</subject><ispartof>Journal of the atmospheric sciences, 2023-02, Vol.80 (2), p.501-517</ispartof><rights>Copyright American Meteorological Society 2023</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c240t-62e7cbab706d69798fed3279c57d7ba52ae121e1cfcefa3c3b87f451cb8ec9763</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Pokrifka, Gwenore F.</creatorcontrib><creatorcontrib>Moyle, Alfred M.</creatorcontrib><creatorcontrib>Harrington, Jerry Y.</creatorcontrib><title>Effective Density Derived from Laboratory Measurements of the Vapor Growth Rates of Small Ice Crystals at −65° to −40°C</title><title>Journal of the atmospheric sciences</title><description>An electrodynamic levitation thermal-gradient diffusion chamber was used to grow 268 individual, small ice particles (initial radii of 8–26
μ
m) from the vapor, at temperatures ranging from −65° to −40°C, and supersaturations up to liquid saturation. Growth limited by attachment kinetics was frequently measured at low supersaturation, as shown in prior work. At high supersaturation, enhanced growth was measured, likely due to the development of branches and hollowed facets. The effects of branching and hollowing on particle growth are often treated with an effective density
ρ
eff
. We fit the measured time series with two different models to estimate size-dependent
ρ
eff
values: the first model decreases
ρ
eff
to an asymptotic deposition density
ρ
dep
, and the second models
ρ
eff
by a power law with exponent
P
. Both methods produce similar results, though the fits with
ρ
dep
typically have lower relative errors. The fit results do not correspond well with models of isometric or planar single-crystalline growth. While single-crystalline columnar crystals correspond to some of the highest growth rates, a newly constructed geometric model of budding rosette crystals produces the best match with the growth data. The relative frequency of occurrence of
ρ
dep
and
P
values show a clear dependence on ice supersaturation normalized to liquid saturation. We use these relative frequencies of
ρ
dep
and
P
to derive two supersaturation-dependent mass–size relationships suitable for cloud modeling applications.</description><subject>Aircraft</subject><subject>Budding</subject><subject>Crystals</subject><subject>Density</subject><subject>Diffusion chambers</subject><subject>Experiments</subject><subject>Growth models</subject><subject>Growth rate</subject><subject>Ice</subject><subject>Ice crystals</subject><subject>Ice particles</subject><subject>Isometric</subject><subject>Kinetics</subject><subject>Laboratories</subject><subject>Levitation</subject><subject>Modelling</subject><subject>Production methods</subject><subject>Saturation</subject><subject>Single crystals</subject><subject>Supersaturation</subject><subject>Time series</subject><subject>Vapors</subject><issn>0022-4928</issn><issn>1520-0469</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNotkM1OAjEUhRujiYiu3TZxPdB2fjqzJAMiBmMi6rbpdG4DhKHYFs0s3Lv2SXgGHsUnsYh3c-7Nd3JuchC6pqRHKU_794NZNIwYiwjhvEdPUIemjEQkyYpT1CEkkKRg-Tm6cG5JwjBOO-hzpDUov3gHPIS1W_g2qA1njbU1DZ7KyljpjW3xA0i3tdDA2jtsNPZzwK9yYyweW_Ph5_hJevgjs0auVniiAJe2dV6uHJYe_3x9Z-l-h705rAnZ78pLdKYDhat_7aKX29FzeRdNH8eTcjCNFEuIjzIGXFWy4iSrs4IXuYY6ZrxQKa95JVMmgTIKVGkFWsYqrnKuk5SqKgdV8Czuoptj7saaty04L5Zma9fhpWA5CZFpkpLg6h9dyhrnLGixsYtG2lZQIg4di9CxGArGxKFjQeNflYxy-A</recordid><startdate>202302</startdate><enddate>202302</enddate><creator>Pokrifka, Gwenore F.</creator><creator>Moyle, Alfred M.</creator><creator>Harrington, Jerry Y.</creator><general>American Meteorological Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8AF</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>M1Q</scope><scope>M2O</scope><scope>M2P</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>R05</scope><scope>S0X</scope></search><sort><creationdate>202302</creationdate><title>Effective Density Derived from Laboratory Measurements of the Vapor Growth Rates of Small Ice Crystals at −65° to −40°C</title><author>Pokrifka, Gwenore F. ; Moyle, Alfred M. ; Harrington, Jerry Y.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c240t-62e7cbab706d69798fed3279c57d7ba52ae121e1cfcefa3c3b87f451cb8ec9763</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Aircraft</topic><topic>Budding</topic><topic>Crystals</topic><topic>Density</topic><topic>Diffusion chambers</topic><topic>Experiments</topic><topic>Growth models</topic><topic>Growth rate</topic><topic>Ice</topic><topic>Ice crystals</topic><topic>Ice particles</topic><topic>Isometric</topic><topic>Kinetics</topic><topic>Laboratories</topic><topic>Levitation</topic><topic>Modelling</topic><topic>Production methods</topic><topic>Saturation</topic><topic>Single crystals</topic><topic>Supersaturation</topic><topic>Time series</topic><topic>Vapors</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pokrifka, Gwenore F.</creatorcontrib><creatorcontrib>Moyle, Alfred M.</creatorcontrib><creatorcontrib>Harrington, Jerry Y.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Agriculture & Environmental Science Database</collection><collection>ProQuest Central Essentials</collection><collection>eLibrary</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Military Database (Proquest) (PQ_SDU_P3)</collection><collection>ProQuest research library</collection><collection>ProQuest Science Journals</collection><collection>Research Library (Corporate)</collection><collection>ProQuest advanced technologies & aerospace journals</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>ProQuest Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>University of Michigan</collection><collection>SIRS Editorial</collection><jtitle>Journal of the atmospheric sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pokrifka, Gwenore F.</au><au>Moyle, Alfred M.</au><au>Harrington, Jerry Y.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effective Density Derived from Laboratory Measurements of the Vapor Growth Rates of Small Ice Crystals at −65° to −40°C</atitle><jtitle>Journal of the atmospheric sciences</jtitle><date>2023-02</date><risdate>2023</risdate><volume>80</volume><issue>2</issue><spage>501</spage><epage>517</epage><pages>501-517</pages><issn>0022-4928</issn><eissn>1520-0469</eissn><abstract>An electrodynamic levitation thermal-gradient diffusion chamber was used to grow 268 individual, small ice particles (initial radii of 8–26
μ
m) from the vapor, at temperatures ranging from −65° to −40°C, and supersaturations up to liquid saturation. Growth limited by attachment kinetics was frequently measured at low supersaturation, as shown in prior work. At high supersaturation, enhanced growth was measured, likely due to the development of branches and hollowed facets. The effects of branching and hollowing on particle growth are often treated with an effective density
ρ
eff
. We fit the measured time series with two different models to estimate size-dependent
ρ
eff
values: the first model decreases
ρ
eff
to an asymptotic deposition density
ρ
dep
, and the second models
ρ
eff
by a power law with exponent
P
. Both methods produce similar results, though the fits with
ρ
dep
typically have lower relative errors. The fit results do not correspond well with models of isometric or planar single-crystalline growth. While single-crystalline columnar crystals correspond to some of the highest growth rates, a newly constructed geometric model of budding rosette crystals produces the best match with the growth data. The relative frequency of occurrence of
ρ
dep
and
P
values show a clear dependence on ice supersaturation normalized to liquid saturation. We use these relative frequencies of
ρ
dep
and
P
to derive two supersaturation-dependent mass–size relationships suitable for cloud modeling applications.</abstract><cop>Boston</cop><pub>American Meteorological Society</pub><doi>10.1175/JAS-D-22-0077.1</doi><tpages>17</tpages><oa>free_for_read</oa></addata></record> |
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issn | 0022-4928 1520-0469 |
language | eng |
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source | EZB Electronic Journals Library |
subjects | Aircraft Budding Crystals Density Diffusion chambers Experiments Growth models Growth rate Ice Ice crystals Ice particles Isometric Kinetics Laboratories Levitation Modelling Production methods Saturation Single crystals Supersaturation Time series Vapors |
title | Effective Density Derived from Laboratory Measurements of the Vapor Growth Rates of Small Ice Crystals at −65° to −40°C |
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