<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-6-493-2006</article-id>
<title-group>
<article-title>NO&lt;sub&gt;2&lt;/sub&gt; Profile Retrieval using airborne multi axis UV-visible skylight absorption measurements over central Europe</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bruns</surname>
<given-names>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>Buehler</surname>
<given-names>S. A.</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>Burrows</surname>
<given-names>J. P.</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>Richter</surname>
<given-names>A.</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>Rozanov</surname>
<given-names>A.</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>Wang</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Heue</surname>
<given-names>K.-P.</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>Platt</surname>
<given-names>U.</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>Pundt</surname>
<given-names>I.</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>Wagner</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Physics, University of Bremen, P.O. Box 33 04 40, 28359 Bremen, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Environmental Physics, University of Heidelberg, Im Neuenheimer Feld 229, 69120 Heidelberg, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>now at: Climate Research and Seismology Department, Royal Netherlands Meteorological Institute (KNMI), P.O. Box 201, 3730 AE De Bilt, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>01</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>1</issue>
<fpage>493</fpage>
<lpage>517</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-discuss.net/6/493/2006/acpd-6-493-2006.html">This article is available from http://www.atmos-chem-phys-discuss.net/6/493/2006/acpd-6-493-2006.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/6/493/2006/acpd-6-493-2006.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/6/493/2006/acpd-6-493-2006.pdf</self-uri>
<abstract>
<p>A recent development in ground-based remote sensing of atmospheric
constituents by UV/visible absorption measurements of scattered
light is the simultaneous use of several directions with small
elevation angles in addition to the traditional zenith-sky pointing.
The different light paths through the atmosphere enable the vertical
distribution of some atmospheric absorbers such as NO&lt;sub&gt;2&lt;/sub&gt;, BrO or
O&lt;sub&gt;3&lt;/sub&gt; to be retrieved.
&lt;br&gt;&lt;br&gt;
In this study, the amount of profile information that can be
retrieved from such measurements on aircraft is investigated for
the trace gas NO&lt;sub&gt;2&lt;/sub&gt;. A Sensitivity study on synthetic data is
performed for a combination of four lines of sight (LOS)
(0&amp;deg; (nadir), 88&amp;deg;, 92&amp;deg;, and
180&amp;deg; (zenith)) and three wavelength regions [center
wavelengths: 362.5&amp;nbsp;nm, 437.5&amp;nbsp;nm, and 485.0&amp;nbsp;nm]. This investigation
demonstrates the potential of this LOS/wavelengths setup to
retrieve a significant amount of profile information from
&lt;B&gt;a&lt;/B&gt;irborne &lt;B&gt;m&lt;/B&gt;ulti&lt;B&gt;ax&lt;/B&gt;is
&lt;B&gt;d&lt;/B&gt;ifferential &lt;B&gt;o&lt;/B&gt;ptical
&lt;B&gt;a&lt;/B&gt;bsorption &lt;B&gt;s&lt;/B&gt;pectrometer (AMAXDOAS)
measurements with a vertical resolution of 3.0 to 4.5&amp;nbsp;km in the
lower troposphere and 2.0 to 3.5&amp;nbsp;km near flight altitude. Above
13&amp;nbsp;km the profile information content of AMAXDOAS measurements is
sparse.
&lt;br&gt;&lt;br&gt;
Further, retrieved profiles with a significant amount (up to
3.2&amp;nbsp;ppbv) of NO&lt;sub&gt;2&lt;/sub&gt; in the boundary layer over the Po-valley
(Italy) are presented. Airborne multiaxis measurements are thus a
promising tool for atmospheric studies in the troposphere.</p>
</abstract>
<counts><page-count count="25"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>