Secondary ice growth mechanism for ice nuclei in the atmosphere
The study of atmospheric ice nuclei is vital for understanding the formation of precipitation and the development of cloud systems as it reveals how these tiny particles grow. A mechanism of such growth when the nuclei are in a mixed ice/water phase and quantum vacuum fluctuation-induced Casimir-Lif...
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creator | Boström, M Li, Y Brevik, I Persson, C Carretero-Palacios, S Malyi, O. I |
description | The study of atmospheric ice nuclei is vital for understanding the formation
of precipitation and the development of cloud systems as it reveals how these
tiny particles grow. A mechanism of such growth when the nuclei are in a mixed
ice/water phase and quantum vacuum fluctuation-induced Casimir-Lifshitz
interaction highlights the complexity and interconnection of the atmospheric
processes with quantum theory. Initially of the order of $0.1\sim10\rm\mu m$ in
size, atmospheric ice nuclei can expand by the accumulation of water molecules
from the surrounding water vapor. |
doi_str_mv | 10.48550/arxiv.2303.05239 |
format | Article |
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of precipitation and the development of cloud systems as it reveals how these
tiny particles grow. A mechanism of such growth when the nuclei are in a mixed
ice/water phase and quantum vacuum fluctuation-induced Casimir-Lifshitz
interaction highlights the complexity and interconnection of the atmospheric
processes with quantum theory. Initially of the order of $0.1\sim10\rm\mu m$ in
size, atmospheric ice nuclei can expand by the accumulation of water molecules
from the surrounding water vapor.</description><identifier>DOI: 10.48550/arxiv.2303.05239</identifier><language>eng</language><subject>Physics - High Energy Physics - Theory ; Physics - Materials Science ; Physics - Statistical Mechanics</subject><creationdate>2023-03</creationdate><rights>http://creativecommons.org/licenses/by-nc-nd/4.0</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>228,230,780,885</link.rule.ids><linktorsrc>$$Uhttps://arxiv.org/abs/2303.05239$$EView_record_in_Cornell_University$$FView_record_in_$$GCornell_University$$Hfree_for_read</linktorsrc><backlink>$$Uhttps://doi.org/10.48550/arXiv.2303.05239$$DView paper in arXiv$$Hfree_for_read</backlink></links><search><creatorcontrib>Boström, M</creatorcontrib><creatorcontrib>Li, Y</creatorcontrib><creatorcontrib>Brevik, I</creatorcontrib><creatorcontrib>Persson, C</creatorcontrib><creatorcontrib>Carretero-Palacios, S</creatorcontrib><creatorcontrib>Malyi, O. I</creatorcontrib><title>Secondary ice growth mechanism for ice nuclei in the atmosphere</title><description>The study of atmospheric ice nuclei is vital for understanding the formation
of precipitation and the development of cloud systems as it reveals how these
tiny particles grow. A mechanism of such growth when the nuclei are in a mixed
ice/water phase and quantum vacuum fluctuation-induced Casimir-Lifshitz
interaction highlights the complexity and interconnection of the atmospheric
processes with quantum theory. Initially of the order of $0.1\sim10\rm\mu m$ in
size, atmospheric ice nuclei can expand by the accumulation of water molecules
from the surrounding water vapor.</description><subject>Physics - High Energy Physics - Theory</subject><subject>Physics - Materials Science</subject><subject>Physics - Statistical Mechanics</subject><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>GOX</sourceid><recordid>eNotz7tOxDAUBFA3FGjhA6jwDyTY8SN2hdCKl7TSFmwfXV9fE0ubZOWE198DgWqKkUZzGLuSotbOGHED5TO_140SqhamUf6c3b4QTmOE8sUzEn8t08fS84GwhzHPA09TWYvxDY-UeR750hOHZZjmU0-FLthZguNMl_-5YYeH-8P2qdrtH5-3d7sKbOsro40LSgqrjXeqhWAVkpAIWlMIjQAfYnDWe2jbZEnGiBhVcmSTDSi92rDrv9lV0J1KHn4ud7-SbpWob8TuQ-4</recordid><startdate>20230309</startdate><enddate>20230309</enddate><creator>Boström, M</creator><creator>Li, Y</creator><creator>Brevik, I</creator><creator>Persson, C</creator><creator>Carretero-Palacios, S</creator><creator>Malyi, O. I</creator><scope>GOX</scope></search><sort><creationdate>20230309</creationdate><title>Secondary ice growth mechanism for ice nuclei in the atmosphere</title><author>Boström, M ; Li, Y ; Brevik, I ; Persson, C ; Carretero-Palacios, S ; Malyi, O. I</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a679-5458b3106459837ab63ce01ca44ebb20a9bdb8699a77f6e1ddccd3f8e6f6bc193</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Physics - High Energy Physics - Theory</topic><topic>Physics - Materials Science</topic><topic>Physics - Statistical Mechanics</topic><toplevel>online_resources</toplevel><creatorcontrib>Boström, M</creatorcontrib><creatorcontrib>Li, Y</creatorcontrib><creatorcontrib>Brevik, I</creatorcontrib><creatorcontrib>Persson, C</creatorcontrib><creatorcontrib>Carretero-Palacios, S</creatorcontrib><creatorcontrib>Malyi, O. I</creatorcontrib><collection>arXiv.org</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Boström, M</au><au>Li, Y</au><au>Brevik, I</au><au>Persson, C</au><au>Carretero-Palacios, S</au><au>Malyi, O. I</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Secondary ice growth mechanism for ice nuclei in the atmosphere</atitle><date>2023-03-09</date><risdate>2023</risdate><abstract>The study of atmospheric ice nuclei is vital for understanding the formation
of precipitation and the development of cloud systems as it reveals how these
tiny particles grow. A mechanism of such growth when the nuclei are in a mixed
ice/water phase and quantum vacuum fluctuation-induced Casimir-Lifshitz
interaction highlights the complexity and interconnection of the atmospheric
processes with quantum theory. Initially of the order of $0.1\sim10\rm\mu m$ in
size, atmospheric ice nuclei can expand by the accumulation of water molecules
from the surrounding water vapor.</abstract><doi>10.48550/arxiv.2303.05239</doi><oa>free_for_read</oa></addata></record> |
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source | arXiv.org |
subjects | Physics - High Energy Physics - Theory Physics - Materials Science Physics - Statistical Mechanics |
title | Secondary ice growth mechanism for ice nuclei in the atmosphere |
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