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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-6-2887-2006</article-id>
<title-group>
<article-title>The time-space exchangeability of satellite retrieved relations between cloud top temperature and particle effective radius</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lensky</surname>
<given-names>I. 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>Rosenfeld</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Geography and Environmental Studies, Bar-Ilan University, Ramat-Gan, Israel</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem, Israel</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>07</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>10</issue>
<fpage>2887</fpage>
<lpage>2894</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>A 3-minute 3-km rapid scan of the METEOSAT Second Generation geostationary
satellite over southern Africa was applied to tracking the evolution of
cloud top temperature (&lt;i&gt;T&lt;/i&gt;) and particle effective radius (&lt;i&gt;r&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt;) of
convective elements. The evolution of &lt;i&gt;T-r&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt; relations showed little
dependence on time, leaving &lt;i&gt;r&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt; to depend almost exclusively on &lt;i&gt;T&lt;/i&gt;.
Furthermore, cloud elements that fully grew to large cumulonimbus stature
had the same &lt;i&gt;T-r&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt; relations as other clouds in the same area with
limited development that decayed without ever becoming a cumulonimbus.
Therefore, a snap shot of &lt;i&gt;T-r&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt; relations over a cloud field provides
the same relations as composed from tracking the time evolution of &lt;i&gt;T&lt;/i&gt; and
&lt;i&gt;r&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt; of individual clouds, and then compositing them. This is the essence
of exchangeability of time and space scales, i.e., ergodicity, of the
&lt;i&gt;T-r&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt; relations for convective clouds. This property has allowed
inference of the microphysical evolution of convective clouds with a snap
shot from a polar orbiter. The fundamental causes for the ergodicity are
suggested to be the observed stability of &lt;i&gt;r&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt; for a given height above
cloud base in a convective cloud, and the constant renewal of growing cloud
tops with cloud bubbles that replace the cloud tops with fresh cloud matter
from below.</p>
</abstract>
<counts><page-count count="8"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</back>
</article>