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Ice nucleus - Wikipedia

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<div class="mw-indicators"> </div> <div id="siteSub" class="noprint">From Wikipedia, the free encyclopedia</div> </div> <div id="contentSub"><div id="mw-content-subtitle"></div></div> <div id="mw-content-text" class="mw-body-content"><div class="mw-content-ltr mw-parser-output" lang="en" dir="ltr"><figure typeof="mw:File/Thumb"><a href="/wiki/File:Ice_Nucleation_Mechanisms.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/3/39/Ice_Nucleation_Mechanisms.png/400px-Ice_Nucleation_Mechanisms.png" decoding="async" width="400" height="280" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/3/39/Ice_Nucleation_Mechanisms.png/600px-Ice_Nucleation_Mechanisms.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/3/39/Ice_Nucleation_Mechanisms.png/800px-Ice_Nucleation_Mechanisms.png 2x" data-file-width="1200" data-file-height="840" /></a><figcaption>Ice nucleation mechanisms describe four modes that are responsible for the formation of primary ice crystals in the atmosphere.<sup class="noprint Inline-Template" style="margin-left:0.1em; white-space:nowrap;">&#91;<i><a href="/wiki/Wikipedia:Please_clarify" title="Wikipedia:Please clarify"><span title="The image is rather vague. More details and legend needed. (July 2019)">clarification needed</span></a></i>&#93;</sup></figcaption></figure> <p>An <b>ice nucleus</b>, also known as an <b>ice nucleating particle</b> (<b>INP</b>), is a particle which acts as the <a href="/wiki/Nucleation" title="Nucleation">nucleus</a> for the formation of an <a href="/wiki/Ice_crystal" title="Ice crystal">ice crystal</a> in the <a href="/wiki/Earth%27s_atmosphere" class="mw-redirect" title="Earth&#39;s atmosphere">atmosphere</a>. </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Ice_nucleation_mechanisms">Ice nucleation mechanisms</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Ice_nucleus&amp;action=edit&amp;section=1" title="Edit section: Ice nucleation mechanisms"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>There are a number of mechanisms of ice nucleation in the atmosphere through which ice nuclei can catalyse the formation of ice particles. In the upper <a href="/wiki/Troposphere" title="Troposphere">troposphere</a>, water vapor can deposit directly onto solid particles. In clouds warmer than about &#8722;37&#160;°C where liquid water can persist in a <a href="/wiki/Supercooling" title="Supercooling">supercooled</a> state, ice nuclei can trigger droplets to freeze.<sup id="cite_ref-Murray2012_1-0" class="reference"><a href="#cite_note-Murray2012-1"><span class="cite-bracket">&#91;</span>1<span class="cite-bracket">&#93;</span></a></sup> </p><p>Contact nucleation can occur if an ice nucleus collides with a supercooled droplet, but the more important mechanism of freezing is when an ice nucleus becomes immersed in a supercooled water droplet and then triggers freezing. </p><p>In the absence of an ice nucleating particle, pure water droplets can persist in a supercooled state to temperatures approaching &#8722;37&#160;°C where they freeze homogeneously.<sup id="cite_ref-Kulkarni2015_2-0" class="reference"><a href="#cite_note-Kulkarni2015-2"><span class="cite-bracket">&#91;</span>2<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Koop2004_3-0" class="reference"><a href="#cite_note-Koop2004-3"><span class="cite-bracket">&#91;</span>3<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Murray2010_4-0" class="reference"><a href="#cite_note-Murray2010-4"><span class="cite-bracket">&#91;</span>4<span class="cite-bracket">&#93;</span></a></sup> </p><p>As per Web of Science, the key word "ice nucleation" that appeared under Met Atm Sci and Env Sci categories till Dec 2021 was plotted using number of papers published. </p> <figure typeof="mw:File/Thumb"><a href="/wiki/File:Growth_of_number_of_papers_with_keyword_Ice_Nucleation.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Growth_of_number_of_papers_with_keyword_Ice_Nucleation.jpg/400px-Growth_of_number_of_papers_with_keyword_Ice_Nucleation.jpg" decoding="async" width="400" height="191" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Growth_of_number_of_papers_with_keyword_Ice_Nucleation.jpg/600px-Growth_of_number_of_papers_with_keyword_Ice_Nucleation.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Growth_of_number_of_papers_with_keyword_Ice_Nucleation.jpg/800px-Growth_of_number_of_papers_with_keyword_Ice_Nucleation.jpg 2x" data-file-width="5510" data-file-height="2625" /></a><figcaption>Growth of number of papers with keyword Ice Nucleation</figcaption></figure> <p>There are several research groups that study ice nucleating properties of atmospheric aerosols (for example see FIN-02 research article by DeMott et al. 2018 or the FIN-02 INP measurement intercomparison study<sup id="cite_ref-DeMott_5-0" class="reference"><a href="#cite_note-DeMott-5"><span class="cite-bracket">&#91;</span>5<span class="cite-bracket">&#93;</span></a></sup>). The ice nucleation research capability is also available through user facility call at EMSL, PNNL.<sup id="cite_ref-6" class="reference"><a href="#cite_note-6"><span class="cite-bracket">&#91;</span>6<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Cloud_dynamics">Cloud dynamics</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Ice_nucleus&amp;action=edit&amp;section=2" title="Edit section: Cloud dynamics"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Ice particles can have a significant effect on <a href="/wiki/Cloud" title="Cloud">cloud</a> dynamics. They are known to be important in the processes by which clouds can become electrified, which causes <a href="/wiki/Lightning" title="Lightning">lightning</a>. They are also known to be able to form the <a href="/wiki/Cloud_seeding" title="Cloud seeding">seeds for rain droplets</a>. It has become clear that the concentration of ice nucleating particles in shallow clouds is a key factor in cloud-climate feedbacks.<sup id="cite_ref-7" class="reference"><a href="#cite_note-7"><span class="cite-bracket">&#91;</span>7<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-8" class="reference"><a href="#cite_note-8"><span class="cite-bracket">&#91;</span>8<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Atmospheric_particulate_matter">Atmospheric particulate matter</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Ice_nucleus&amp;action=edit&amp;section=3" title="Edit section: Atmospheric particulate matter"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Many different types of <a href="/wiki/Atmospheric_particulate_matter" class="mw-redirect" title="Atmospheric particulate matter">atmospheric particulate matter</a> can act as ice nuclei, both natural and anthropogenic, including those composed of desert dust, soot, organic matter, bacteria (e.g. <i><a href="/wiki/Pseudomonas_syringae" title="Pseudomonas syringae">Pseudomonas syringae</a></i>), pollen, fungal spores and volcanic ash amongst others.<sup id="cite_ref-Murray2012_1-1" class="reference"><a href="#cite_note-Murray2012-1"><span class="cite-bracket">&#91;</span>1<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-pmid18309078_9-0" class="reference"><a href="#cite_note-pmid18309078-9"><span class="cite-bracket">&#91;</span>9<span class="cite-bracket">&#93;</span></a></sup> However, the exact <a href="/wiki/Nucleation" title="Nucleation">nucleation</a> potential of each type varies greatly, depending on the exact atmospheric conditions. Very little is known about the spatial distribution of these particles, their overall importance for global climate through ice cloud formation, and whether human activity has played a major role in changing these effects. </p> <div class="mw-heading mw-heading2"><h2 id="See_also">See also</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Ice_nucleus&amp;action=edit&amp;section=4" title="Edit section: See also"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <ul><li><a href="/wiki/Bergeron_process" class="mw-redirect" title="Bergeron process">Bergeron process</a></li> <li><a href="/wiki/Cloud_condensation_nuclei" title="Cloud condensation nuclei">Cloud condensation nuclei</a></li> <li><a href="/wiki/Nucleation" title="Nucleation">Nucleation</a></li> <li><a href="/wiki/Snow" title="Snow">Snow</a></li> <li><a href="/wiki/Supercooling" title="Supercooling">Supercooling</a></li></ul> <div class="mw-heading mw-heading2"><h2 id="References">References</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Ice_nucleus&amp;action=edit&amp;section=5" title="Edit section: References"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1239543626">.mw-parser-output .reflist{margin-bottom:0.5em;list-style-type:decimal}@media screen{.mw-parser-output .reflist{font-size:90%}}.mw-parser-output .reflist .references{font-size:100%;margin-bottom:0;list-style-type:inherit}.mw-parser-output .reflist-columns-2{column-width:30em}.mw-parser-output .reflist-columns-3{column-width:25em}.mw-parser-output .reflist-columns{margin-top:0.3em}.mw-parser-output .reflist-columns ol{margin-top:0}.mw-parser-output .reflist-columns li{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .reflist-upper-alpha{list-style-type:upper-alpha}.mw-parser-output .reflist-upper-roman{list-style-type:upper-roman}.mw-parser-output .reflist-lower-alpha{list-style-type:lower-alpha}.mw-parser-output .reflist-lower-greek{list-style-type:lower-greek}.mw-parser-output .reflist-lower-roman{list-style-type:lower-roman}</style><div class="reflist"> <div class="mw-references-wrap"><ol class="references"> <li id="cite_note-Murray2012-1"><span class="mw-cite-backlink">^ <a href="#cite_ref-Murray2012_1-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-Murray2012_1-1"><sup><i><b>b</b></i></sup></a></span> <span class="reference-text"><style data-mw-deduplicate="TemplateStyles:r1238218222">.mw-parser-output cite.citation{font-style:inherit;word-wrap:break-word}.mw-parser-output .citation q{quotes:"\"""\"""'""'"}.mw-parser-output .citation:target{background-color:rgba(0,127,255,0.133)}.mw-parser-output .id-lock-free.id-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/6/65/Lock-green.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-limited.id-lock-limited a,.mw-parser-output .id-lock-registration.id-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/d/d6/Lock-gray-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-subscription.id-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/a/aa/Lock-red-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .cs1-ws-icon a{background:url("//upload.wikimedia.org/wikipedia/commons/4/4c/Wikisource-logo.svg")right 0.1em center/12px no-repeat}body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-free a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-limited a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-registration a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-subscription a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .cs1-ws-icon a{background-size:contain;padding:0 1em 0 0}.mw-parser-output .cs1-code{color:inherit;background:inherit;border:none;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;color:var(--color-error,#d33)}.mw-parser-output .cs1-visible-error{color:var(--color-error,#d33)}.mw-parser-output .cs1-maint{display:none;color:#085;margin-left:0.3em}.mw-parser-output .cs1-kern-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right{padding-right:0.2em}.mw-parser-output .citation .mw-selflink{font-weight:inherit}@media screen{.mw-parser-output .cs1-format{font-size:95%}html.skin-theme-clientpref-night .mw-parser-output .cs1-maint{color:#18911f}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .cs1-maint{color:#18911f}}</style><cite id="CITEREFMurray2012" class="citation journal cs1">Murray; et&#160;al. 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(13 March 2018). <a rel="nofollow" class="external text" href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5856555">"Strong control of Southern Ocean cloud reflectivity by ice-nucleating particles"</a>. <i>Proceedings of the National Academy of Sciences</i>. <b>115</b> (11): 2687–2692. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2018PNAS..115.2687V">2018PNAS..115.2687V</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<span class="id-lock-free" title="Freely accessible"><a rel="nofollow" class="external text" href="https://doi.org/10.1073%2Fpnas.1721627115">10.1073/pnas.1721627115</a></span>. <a href="/wiki/PMC_(identifier)" class="mw-redirect" title="PMC (identifier)">PMC</a>&#160;<span class="id-lock-free" title="Freely accessible"><a rel="nofollow" class="external text" href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5856555">5856555</a></span>. <a href="/wiki/PMID_(identifier)" class="mw-redirect" title="PMID (identifier)">PMID</a>&#160;<a rel="nofollow" class="external text" href="https://pubmed.ncbi.nlm.nih.gov/29490918">29490918</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=article&amp;rft.jtitle=Proceedings+of+the+National+Academy+of+Sciences&amp;rft.atitle=Strong+control+of+Southern+Ocean+cloud+reflectivity+by+ice-nucleating+particles&amp;rft.volume=115&amp;rft.issue=11&amp;rft.pages=2687-2692&amp;rft.date=2018-03-13&amp;rft_id=https%3A%2F%2Fwww.ncbi.nlm.nih.gov%2Fpmc%2Farticles%2FPMC5856555%23id-name%3DPMC&amp;rft_id=info%3Apmid%2F29490918&amp;rft_id=info%3Adoi%2F10.1073%2Fpnas.1721627115&amp;rft_id=info%3Abibcode%2F2018PNAS..115.2687V&amp;rft.aulast=Vergara-Temprado&amp;rft.aufirst=Jes%C3%BAs&amp;rft.au=Miltenberger%2C+Annette+K.&amp;rft.au=Furtado%2C+Kalli&amp;rft.au=Grosvenor%2C+Daniel+P.&amp;rft.au=Shipway%2C+Ben+J.&amp;rft.au=Hill%2C+Adrian+A.&amp;rft.au=Wilkinson%2C+Jonathan+M.&amp;rft.au=Field%2C+Paul+R.&amp;rft.au=Murray%2C+Benjamin+J.&amp;rft.au=Carslaw%2C+Ken+S.&amp;rft_id=https%3A%2F%2Fwww.ncbi.nlm.nih.gov%2Fpmc%2Farticles%2FPMC5856555&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3AIce+nucleus" class="Z3988"></span></span> </li> <li id="cite_note-pmid18309078-9"><span class="mw-cite-backlink"><b><a href="#cite_ref-pmid18309078_9-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFChristnerMorrisForemanCai2008" class="citation journal cs1">Christner BC, Morris CE, Foreman CM, Cai R, Sands DC (2008). "Ubiquity of biological ice nucleators in snowfall". <i><a href="/wiki/Science_(journal)" title="Science (journal)">Science</a></i>. <b>319</b> (5867): 1214. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2008Sci...319.1214C">2008Sci...319.1214C</a>. <a href="/wiki/CiteSeerX_(identifier)" class="mw-redirect" title="CiteSeerX (identifier)">CiteSeerX</a>&#160;<span class="id-lock-free" title="Freely accessible"><a rel="nofollow" class="external text" href="https://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.4918">10.1.1.395.4918</a></span>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1126%2Fscience.1149757">10.1126/science.1149757</a>. <a href="/wiki/PMID_(identifier)" class="mw-redirect" title="PMID (identifier)">PMID</a>&#160;<a rel="nofollow" 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class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Phases_of_ice#Amorphous_ice" title="Phases of ice">Amorphous solid</a></li> <li><a href="/wiki/Phases_of_ice#Known_phases" title="Phases of ice">Crystalline phases</a></li> <li><a href="/wiki/Phases_of_ice#Ice_XVIII_(superionic_water)" title="Phases of ice">Superionic</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Formations</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Anchor_ice" title="Anchor ice">Anchor</a></li> <li><a href="/wiki/Ice_cap" title="Ice cap">Cap</a></li> <li><a href="/wiki/Ice_cave" title="Ice cave">Cave</a></li> <li><a href="/wiki/Ice_dune" title="Ice dune">Dune</a></li> <li><a href="/wiki/Ice_field" title="Ice field">Field</a></li> <li><a href="/wiki/Glacier" title="Glacier">Glacier</a></li> <li><a href="/wiki/Iceberg" title="Iceberg">Iceberg</a>&#160;(<a href="/wiki/Ice_calving" title="Ice calving">calving</a>)</li> <li><a href="/wiki/Icicle" title="Icicle">Icicle</a></li> <li><a href="/wiki/Ice_jam" title="Ice jam">Jam</a></li> <li><a href="/wiki/Sea_ice" title="Sea ice">Sea</a></li> <li><a href="/wiki/Ice_sheet" title="Ice sheet">Sheet</a></li> <li><a href="/wiki/Ice_spike" title="Ice spike">Spike</a></li> <li><a href="/wiki/Stalactite#Ice_stalactites" title="Stalactite">Stalactites</a></li> <li><a href="/wiki/Ice_volcano" title="Ice volcano">Volcano</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Phenomena</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Ice%E2%80%93albedo_feedback" title="Ice–albedo feedback">Albedo feedback</a></li> <li><a href="/wiki/Black_ice" title="Black ice">Black</a></li> <li><a href="/wiki/Ice_circle" title="Ice circle">Circle or disc</a></li> <li><a href="/wiki/Clear_ice" title="Clear ice">Clear</a></li> <li><a href="/wiki/Ice_crystals" class="mw-redirect" title="Ice crystals">Crystals</a></li> <li><a href="/wiki/Firn" title="Firn">Firn</a></li> <li><a href="/wiki/Ice_fog" class="mw-redirect" title="Ice fog">Fog</a></li> <li><a href="/wiki/Frazil_ice" title="Frazil ice">Frazil</a></li> <li><a href="/wiki/Frost" title="Frost">Frost</a></li> <li><a href="/wiki/Frost_heaving" title="Frost heaving">Frost heave</a></li> <li><a href="/wiki/Frost_flower" title="Frost flower">Frost flower</a>&#160;(<a href="/wiki/Frost_flower_(sea_ice)" title="Frost flower (sea ice)">sea ice</a>)</li> <li><a href="/wiki/Glaze_(ice)" title="Glaze (ice)">Glaze</a></li> <li><a href="/wiki/Hail" title="Hail">Hail</a></li> <li><a href="/wiki/Hair_ice" title="Hair ice">Hair ice</a></li> <li><a href="/wiki/Ice_jacking" title="Ice jacking">Jacking</a></li> <li><a href="/wiki/N%C3%A9v%C3%A9" title="Névé">Névé</a></li> <li><a href="/wiki/Needle_ice" title="Needle ice">Needle</a></li> <li><a class="mw-selflink selflink">Nucleus</a></li> <li><a href="/wiki/Rime_ice" title="Rime ice">Rime</a></li> <li><a href="/wiki/Ice_shove" title="Ice shove">Shove</a></li> <li><a href="/wiki/Shuga_(ice)" title="Shuga (ice)">Shuga</a></li> <li><a href="/wiki/Slurry_ice" title="Slurry ice">Slurry</a></li> <li><a href="/wiki/Slush" title="Slush">Slush</a></li> <li><a href="/wiki/Snow" title="Snow">Snow</a></li> <li><a href="/wiki/Ice_storm" title="Ice storm">Storm</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Ice-related<br />activities</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><td colspan="2" class="navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Ice_bath" title="Ice bath">Bathing</a></li> <li><a href="/wiki/Ice_blasting" title="Ice blasting">Blasting</a></li> <li><a href="/wiki/Ice_blocking" title="Ice blocking">Blocking</a></li> <li><a href="/wiki/Ice_climbing" title="Ice climbing">Climbing</a></li> <li><a href="/wiki/Ice_fishing" title="Ice fishing">Fishing</a></li> <li><a href="/wiki/Ice_rafting" title="Ice rafting">Rafting</a></li> <li><a href="/wiki/Ice_sculpture" title="Ice sculpture">Sculpture</a></li> <li><a href="/wiki/Ice_skating" title="Ice skating">Skating</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%;font-weight: normal;"><a href="/wiki/Winter_sports" title="Winter sports">Sports</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Bandy" title="Bandy">Bandy</a></li> <li><a href="/wiki/Iceboat" title="Iceboat">Iceboating</a></li> <li><a href="/wiki/Ice_cricket" title="Ice cricket">Cricket</a></li> <li><a href="/wiki/Curling" title="Curling">Curling</a></li> <li><a href="/wiki/Icetrack_cycling" title="Icetrack cycling">Cycling</a></li> <li><a href="/wiki/Figure_skating" title="Figure skating">Figure skating</a></li> <li><a href="/wiki/Ice_hockey" title="Ice hockey">Ice hockey</a></li> <li><a href="/wiki/Ice_racing" title="Ice racing">Ice racing</a></li> <li><a href="/wiki/Speed_skating" title="Speed skating">Speed skating</a></li> <li><a href="/wiki/Short-track_speed_skating" title="Short-track speed skating">Short-track speed skating</a></li> <li><a href="/wiki/Tour_skating" title="Tour skating">Tour skating</a></li></ul> </div></td></tr></tbody></table><div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Constructions</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Ice_bar" title="Ice 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