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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</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/acp-14-1055-2014</article-id>
<title-group>
<article-title>Nitric acid trihydrate nucleation and denitrification in the Arctic stratosphere</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Grooß</surname>
<given-names>J.-U.</given-names>
<ext-link>https://orcid.org/0000-0002-9485-866X</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Engel</surname>
<given-names>I.</given-names>
<ext-link>https://orcid.org/0000-0001-5285-7952</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Borrmann</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Frey</surname>
<given-names>W.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff12">
<sup>12</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Günther</surname>
<given-names>G.</given-names>
<ext-link>https://orcid.org/0000-0003-4111-6221</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hoyle</surname>
<given-names>C. R.</given-names>
<ext-link>https://orcid.org/0000-0002-1369-9143</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kivi</surname>
<given-names>R.</given-names>
<ext-link>https://orcid.org/0000-0001-8828-2759</ext-link>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Luo</surname>
<given-names>B. 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>Molleker</surname>
<given-names>S.</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>Peter</surname>
<given-names>T.</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>Pitts</surname>
<given-names>M. C.</given-names>
<ext-link>https://orcid.org/0000-0001-8240-7223</ext-link>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Schlager</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Stiller</surname>
<given-names>G.</given-names>
<ext-link>https://orcid.org/0000-0003-2883-6873</ext-link>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vömel</surname>
<given-names>H.</given-names>
<ext-link>https://orcid.org/0000-0003-1223-3429</ext-link>
</name>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Walker</surname>
<given-names>K. A.</given-names>
<ext-link>https://orcid.org/0000-0003-3420-9454</ext-link>
</name>
<xref ref-type="aff" rid="aff11">
<sup>11</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Müller</surname>
<given-names>R.</given-names>
<ext-link>https://orcid.org/0000-0002-5024-9977</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institut für Energie- und Klimaforschung &amp;ndash; Stratosphäre (IEK-7),  Forschungszentrum Jülich, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institut für Physik der Atmosphäre, Johannes-Gutenberg-Universität  Mainz, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Abteilung Partikelchemie, Max Planck Institut für Chemie,  Mainz, Germany</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Paul Scherrer Institute, Villigen, Switzerland</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Finnish Meteorological Institute, Sodankylä, Finnland</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>NASA Langley Research Center, Hampton, VA, USA</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Institut für Physik der Atmosphäre,  Deutsches Zentrum für Luft- und Raumfahrt, Oberpfaffenhofen, Germany</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>Institute for Meteorology and Climate Research, Karlsruhe  Institute of Technology, Karlsruhe, Germany</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>Meteorological Observatory Lindenberg, Deutscher Wetterdienst, Germany</addr-line>
</aff>
<aff id="aff11">
<label>11</label>
<addr-line>Department of Physics, University of Toronto, Ontario, Canada</addr-line>
</aff>
<aff id="aff12">
<label>12</label>
<addr-line>now at: School of Earth Sciences, The University of Melbourne,  Melbourne, Australia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>01</month>
<year>2014</year>
</pub-date>
<volume>14</volume>
<issue>2</issue>
<fpage>1055</fpage>
<lpage>1073</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 J.-U. Grooß et al.</copyright-statement>
<copyright-year>2014</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>
<self-uri xlink:href="https://acp.copernicus.org/articles/14/1055/2014/acp-14-1055-2014.html">This article is available from https://acp.copernicus.org/articles/14/1055/2014/acp-14-1055-2014.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/14/1055/2014/acp-14-1055-2014.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/14/1055/2014/acp-14-1055-2014.pdf</self-uri>
<abstract>
<p>Nitric acid trihydrate (NAT) particles in the polar stratosphere have been
shown to be responsible for vertical redistribution of reactive nitrogen
(NO&lt;sub&gt;y&lt;/sub&gt;). Recent observations by Cloud–Aerosol Lidar with Orthogonal
Polarization (CALIOP) aboard the CALIPSO satellite have been explained in
terms of heterogeneous nucleation of NAT on foreign nuclei, revealing this to
be an important formation pathway for the NAT particles. In state of the art
global- or regional-scale models, heterogeneous NAT nucleation is currently
simulated in a very coarse manner using a constant, saturation-independent
nucleation rate. Here we present first simulations for the Arctic winter
2009/2010 applying a new saturation-dependent parametrisation of
heterogeneous NAT nucleation rates within the Chemical Lagrangian Model of
the Stratosphere (CLaMS). The simulation shows good agreement of chemical
trace species with in situ and remote sensing observations. The simulated polar stratospheric cloud (PSC)
optical properties agree much better with CALIOP observations than those
simulated with a constant nucleation rate model. A comparison of the
simulated particle size distributions with observations made using the
Forward Scattering Spectrometer Probe (FSSP) aboard the high altitude
research aircraft Geophysica, shows that the model reproduces the observed
size distribution, except for the very largest particles above 15 &amp;mu;m diameter. The vertical NO&lt;sub&gt;y&lt;/sub&gt; redistribution caused by the
sedimentation of the NAT particles, in particular the denitrification and
nitrification signals observed by the ACE-FTS satellite instrument and the
in situ SIOUX instrument aboard the Geophysica, are reproduced by the
improved model, and a small improvement with respect to the constant
nucleation rate model is found.</p>
</abstract>
<counts><page-count count="19"/></counts>
<funding-group>
<award-group id="gs1">
<funding-source>European Commission</funding-source>
<award-id>RECONCILE - Reconciliation of essential process parameters for an enhanced predictability of arctic stratospheric ozone loss and its climate interactions. (226365)</award-id>
</award-group>
</funding-group>
</article-meta>
</front>
<body/>
<back>
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