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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-22331-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/22331/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/22331/2009/acpd-9-22331-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/22331/2009/acpd-9-22331-2009.pdf</fulltext_pdf>
	<start_page>22331</start_page>
	<end_page>22336</end_page>
	<publication_date>2009-10-22</publication_date>
	<article_title content_type="html">Comment on &quot;Reinterpreting aircraft measurements in anisotropic scaling turbulence&quot; by Lovejoy et al. (2009)</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. Lindborg</name>
			<email>erikl@mech.kth.se</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>K. K. Tung</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>G. D. Nastrom</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>J. Y. N. Cho</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>K. S. Gage</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Linné Flow Centre, KTH Mechanics, 10044 Stockholm, Sweden</affiliation>
		<affiliation numeration="2" content_type="html">Department of Applied Mathematics, University of Washington, Seattle, WA, USA</affiliation>
		<affiliation numeration="3" content_type="html">St. Cloud State University, St. Cloud, MN, USA</affiliation>
		<affiliation numeration="4" content_type="html">MIT Lincoln Laboratory, Lexington, MA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Cooperative Institute for the Environmental Sciences, Univ. of Colorado, Boulder, CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">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;#x2273;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.</abstract>
	<references>
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</article>

