Experiments on ice spikes and a simple growth model
Ice-spike observations in nature have sparked much interest in the scientific and non-scientific communities alike, yet most research performed thus far has been largely qualitative. We have conducted a quantitative, systematic laboratory investigation in order to assess theories explaining ice-spik...
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Veröffentlicht in: | Journal of glaciology 2004, Vol.50 (170), p.375-381 |
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creator | Hill, Lesley Lozowski, Edward Sampson, Russell D. |
description | Ice-spike observations in nature have sparked much interest in the scientific and non-scientific communities alike, yet most research performed thus far has been largely qualitative. We have conducted a quantitative, systematic laboratory investigation in order to assess theories explaining ice-spike growth and to determine the conditions conducive to it. We observed ice-spike growth using time-lapse digital photography, using two water types in two different containers. We observed that ice spikes occurred much more frequently in distilled water than in tap water. Digital images were analyzed to determine the growth rate of the ice spikes. Water temperature was recorded throughout the freezing process, and the cooling rate was used to estimate a bulk heat transfer coefficient. Finally, a simple model, based on mass conservation, was derived and was found to give useful predictions of ice-spike growth rate. |
doi_str_mv | 10.3189/172756504781829954 |
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We have conducted a quantitative, systematic laboratory investigation in order to assess theories explaining ice-spike growth and to determine the conditions conducive to it. We observed ice-spike growth using time-lapse digital photography, using two water types in two different containers. We observed that ice spikes occurred much more frequently in distilled water than in tap water. Digital images were analyzed to determine the growth rate of the ice spikes. Water temperature was recorded throughout the freezing process, and the cooling rate was used to estimate a bulk heat transfer coefficient. 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Glaciol</addtitle><description>Ice-spike observations in nature have sparked much interest in the scientific and non-scientific communities alike, yet most research performed thus far has been largely qualitative. We have conducted a quantitative, systematic laboratory investigation in order to assess theories explaining ice-spike growth and to determine the conditions conducive to it. We observed ice-spike growth using time-lapse digital photography, using two water types in two different containers. We observed that ice spikes occurred much more frequently in distilled water than in tap water. Digital images were analyzed to determine the growth rate of the ice spikes. Water temperature was recorded throughout the freezing process, and the cooling rate was used to estimate a bulk heat transfer coefficient. Finally, a simple model, based on mass conservation, was derived and was found to give useful predictions of ice-spike growth rate.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Snow. Ice. 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Ice. Glaciers</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hill, Lesley</creatorcontrib><creatorcontrib>Lozowski, Edward</creatorcontrib><creatorcontrib>Sampson, Russell D.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Journal of glaciology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hill, Lesley</au><au>Lozowski, Edward</au><au>Sampson, Russell D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Experiments on ice spikes and a simple growth model</atitle><jtitle>Journal of glaciology</jtitle><addtitle>J. Glaciol</addtitle><date>2004</date><risdate>2004</risdate><volume>50</volume><issue>170</issue><spage>375</spage><epage>381</epage><pages>375-381</pages><issn>0022-1430</issn><eissn>1727-5652</eissn><coden>JOGLAO</coden><abstract>Ice-spike observations in nature have sparked much interest in the scientific and non-scientific communities alike, yet most research performed thus far has been largely qualitative. We have conducted a quantitative, systematic laboratory investigation in order to assess theories explaining ice-spike growth and to determine the conditions conducive to it. We observed ice-spike growth using time-lapse digital photography, using two water types in two different containers. We observed that ice spikes occurred much more frequently in distilled water than in tap water. Digital images were analyzed to determine the growth rate of the ice spikes. Water temperature was recorded throughout the freezing process, and the cooling rate was used to estimate a bulk heat transfer coefficient. Finally, a simple model, based on mass conservation, was derived and was found to give useful predictions of ice-spike growth rate.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.3189/172756504781829954</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Earth, ocean, space Exact sciences and technology External geophysics Snow. Ice. Glaciers |
title | Experiments on ice spikes and a simple growth model |
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