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<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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-2022-104</article-id>
<title-group>
<article-title>Measurement Report: Real-Time Remote Sensing of the Coastal Boundary Layer and its Interaction with Meteorology at Cape Grim, Australia</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chen</surname>
<given-names>Zhenyi</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>Schofield</surname>
<given-names>Robyn</given-names>
<ext-link>https://orcid.org/0000-0002-4230-717X</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Keywood</surname>
<given-names>Melita</given-names>
<ext-link>https://orcid.org/0000-0001-9953-6806</ext-link>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cleland</surname>
<given-names>Sam</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>Williams</surname>
<given-names>Alastair G.</given-names>
<ext-link>https://orcid.org/0000-0002-0568-8487</ext-link>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Griffiths</surname>
<given-names>Alan</given-names>
<ext-link>https://orcid.org/0000-0003-1135-1810</ext-link>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wilson</surname>
<given-names>Stephen</given-names>
<ext-link>https://orcid.org/0000-0003-4546-2527</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>Rayner</surname>
<given-names>Peter</given-names>
<ext-link>https://orcid.org/0000-0001-7707-6298</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Shu</surname>
<given-names>Xiaowen</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Ecology and Environment, Beijing Technology and Business University, 100048, Beijing, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>School of Earth Sciences, University of Melbourne, 3010, Melbourne, VIC, Australia</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Climate Science Centre, Oceans and Atmosphere, CSIRO, 3195, Aspendale, VIC, Australia</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Observing Systems and Operations, Bureau of Meteorology, 7330, Smithton, Tasmania, Australia</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Australian Nuclear Science and Technology Organisation, Lucas Heights, New South Wales, Australia</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>School of Earth, Atmosphere and Life Sciences, University of Wollongong, 2522, NSW, Australia</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, 230031, Hefei, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>03</month>
<year>2022</year>
</pub-date>
<volume>2022</volume>
<fpage>1</fpage>
<lpage>21</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2022 Zhenyi Chen et al.</copyright-statement>
<copyright-year>2022</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/preprints/acp-2022-104/">This article is available from https://acp.copernicus.org/preprints/acp-2022-104/</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/acp-2022-104/acp-2022-104.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/acp-2022-104/acp-2022-104.pdf</self-uri>
<abstract>
<p>&lt;p&gt;Despite considerable efforts during the last decade, real-time characterization of the marine boundary layer and aerosol optical properties over the Southern Ocean remains scarce. We conducted simultaneous measurements of the marine boundary layer utilizing a synergy of remote sensing technology at the Baseline Air Pollution Station at Cape Grim in northwestern Tasmania, Australia, from 14 May to 16 July 2019. Aerosol optical properties were monitored by lidar (miniMPL) and a ceilometer to identify the boundary layer height, and sodar provided wind profiles to investigate their influences on the layer evolution. Boundary layer heights simulated using the Weather Research and Forecasting (WRF) model were also employed for comparison purposes. Through complementary analyses of three cases representing different source influences (marine, sea breeze and continental), this paper evaluates two algorithms (Image Edge Detection Algorithm (IEDA) and gradient method) for boundary layer height detection and examines the vertical aerosol distribution within the boundary layer at Cape Grim with an emphasis on the contributions of regional and local meteorology. We found IEDA generally performed better than the gradient method, especially during the marine-flow-influenced period with a convective layer structure. Different features of boundary layer structures in three episodes, including differential boundary layer growth and interaction with wind evolutionary processes were investigated. One was characterized by a diurnal variation with a boundary layer height of approximately 0.2&amp;ndash;0.5 km, associated with the veering of the wind vector within the marine boundary layer during the development of a sea breeze. The other showed a thermally stable layer below 0.3 km with an enhanced extinction coefficient and linear depolarization ratio under the influence of continental sources, which was also validated by the observation from Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) satellite. The increasing extinction coefficient and depolarization ratio with wind speeds may be attributed to the increased wet sea salt production and regional transportation from mainland Australia.&lt;/p&gt;</p>
</abstract>
<counts><page-count count="21"/></counts>
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