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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-10-1401-2010</article-id>
<title-group>
<article-title>Comment on &quot;Reinterpreting aircraft measurement in anisotropic scaling turbulence&quot; by Lovejoy et al. (2009)</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lindborg</surname>
<given-names>E.</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>Tung</surname>
<given-names>K. K.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nastrom</surname>
<given-names>G. D.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cho</surname>
<given-names>J. Y.  N.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gage</surname>
<given-names>K. S.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Linné Flow Centre, KTH Mechanics, 10044 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Applied Mathematics, University of Washington, Seattle, Washington, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>St. Cloud State University, St. Cloud, Minnesota, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>MIT Lincoln Laboratory, Lexington, Massachusetts, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Cooperative Institute for the Environmental Sciences, University of Colorado, Boulder, Colorado, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>08</day>
<month>02</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>3</issue>
<fpage>1401</fpage>
<lpage>1402</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>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/1401/2010/acp-10-1401-2010.html">This article is available from http://www.atmos-chem-phys.net/10/1401/2010/acp-10-1401-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/1401/2010/acp-10-1401-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/1401/2010/acp-10-1401-2010.pdf</self-uri>
<abstract>
<p>Recently, Lovejoy et al. (2009) argued that the steep ~&lt;i&gt;k&lt;/i&gt;&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
atmospheric kinetic energy spectrum at synoptic scales (&amp;ge;1000 km)
observed by aircraft is a spurious artefact of aircraft following isobars
instead of isoheights. Without taking into account the earth&apos;s rotation they
hypothesise that the horizontal atmospheric energy spectrum should scale as
&lt;i&gt;k&lt;/i&gt;&lt;sup&gt;&amp;minus;5/3&lt;/sup&gt; at all scales. We point out that the approximate &lt;i&gt;k&lt;/i&gt;&lt;sup&gt;&amp;minus;3&lt;/sup&gt;-spectrum
at synoptic scales has been observed by a number of non-aircraft means since the
1960s and that general circulation models and other current models have successfully
produced this spectrum. We also argue that
the vertical movements of the aircraft are far too small to cause any strong
effect on the measured spectrum at synoptic scales.</p>
</abstract>
<counts><page-count count="2"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>