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<front>
<journal-meta>
<journal-id journal-id-type="publisher">AMT</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMT</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8548</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/amt-6-1761-2013</article-id>
<title-group>
<article-title>Calibration and validation of the advanced E-Region Wind Interferometer</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kristoffersen</surname>
<given-names>S. K.</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>Ward</surname>
<given-names>W. 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>Brown</surname>
<given-names>S.</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>Drummond</surname>
<given-names>J. R.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physics, University of New Brunswick, Fredericton, NB, E3B 5A3, Canada</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>CRESS Space Instrumentation Laboratory CSIL, York University, 4700 Keele St. Toronto, ON, M3J 1P3, Canada</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Physics and Atmospheric Science, Dalhousie University, Halifax, NS, B3H 4R2, Canada</addr-line>
</aff>
<pub-date pub-type="epub">
<day>23</day>
<month>07</month>
<year>2013</year>
</pub-date>
<volume>6</volume>
<issue>7</issue>
<fpage>1761</fpage>
<lpage>1776</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 S. K. Kristoffersen et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
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<self-uri xlink:href="https://amt.copernicus.org/articles/6/1761/2013/amt-6-1761-2013.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/articles/6/1761/2013/amt-6-1761-2013.pdf</self-uri>
<abstract>
<p>The advanced E-Region Wind Interferometer (ERWIN II) combines the imaging
capabilities of a CCD detector with the wide field associated with field-widened Michelson interferometry. This instrument is capable of simultaneous
multi-directional wind observations for three different airglow emissions
(oxygen green line (O(&lt;sup&gt;1&lt;/sup&gt;S)) at a height of ~97 km, the
&lt;sup&gt;P&lt;/sup&gt;Q(7) and &lt;sup&gt;P&lt;/sup&gt;(7) emission lines in the O&lt;sub&gt;2&lt;/sub&gt;(0–1) atmospheric
band at ~93 km and P&lt;sub&gt;1&lt;/sub&gt;(3) emission line in the (6, 2)
hydroxyl Meinel band at ~87 km) on a three minute cadence. In
each direction, for 45 s measurements for typical airglow volume
emission rates, the instrument is capable of line-of-sight wind precisions of
~1 m s&lt;sup&gt;−1&lt;/sup&gt; for hydroxyl and O(&lt;sup&gt;1&lt;/sup&gt;S) and ~4 m s&lt;sup&gt;−1&lt;/sup&gt;
for O&lt;sub&gt;2&lt;/sub&gt;. This precision is achieved using a new data analysis algorithm
which takes advantage of the imaging capabilities of the CCD detector along
with knowledge of the instrument phase variation as a function of pixel
location across the detector. This instrument is currently located in
Eureka, Nunavut as part of the Polar Environment Atmospheric Research
Laboratory (PEARL) (80°N, 86° W). The details of the physical configuration,
the data analysis algorithm, the measurement calibration and validation of
the observations from December 2008 and January 2009 are described. Field
measurements which demonstrate the capabilities of this instrument are
presented. To our knowledge, the wind determinations with this instrument
are the most accurate and have the highest observational cadence for airglow
wind observations of this region of the atmosphere and match the
capabilities of other wind-measuring techniques.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>