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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-10-2927-2010</article-id>
<title-group>
<article-title>Scanning electron microscopy and molecular dynamics of surfaces of growing and ablating hexagonal ice crystals</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pfalzgraff</surname>
<given-names>W. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hulscher</surname>
<given-names>R. M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Neshyba</surname>
<given-names>S. P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>University of Puget Sound, Tacoma, Washington, 98416, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>03</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>6</issue>
<fpage>2927</fpage>
<lpage>2935</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<abstract>
<p>We present the first clearly resolved observations of
surfaces of growing and ablating hexagonal ice crystals using
variable-pressure scanning electron microscopy. The ice surface develops
trans-prismatic strands, separated from one another by distances of 5â€“10 &amp;mu;m.
The strands are present at a wide range of supersaturations, but
are most pronounced at temperatures near the frost point. Pyramidal facets
consistent with Miller-Bravais indices of 10&lt;span style=&quot;border-top: 1px solid #000; color: #000;&quot;&gt;1&lt;/span&gt;1, and possibly also 20&lt;span style=&quot;border-top: 1px solid #000; color: #000;&quot;&gt;2&lt;/span&gt;1, 
are associated with ice growth under these conditions. A
molecular-dynamics model of a free-standing ice &lt;i&gt;I&lt;/i&gt;&lt;sub&gt;h&lt;/sub&gt; nanocolumn containing
8400 water molecules does not develop trans-prismatic strands, suggesting
these features originate at larger spatial or temporal scales. The possible
relevance of these surface features to cirrus ice is discussed.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
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