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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-9-21717-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/21717/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/21717/2009/acpd-9-21717-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/21717/2009/acpd-9-21717-2009.pdf</fulltext_pdf>
	<start_page>21717</start_page>
	<end_page>21783</end_page>
	<publication_date>2009-10-15</publication_date>
	<article_title content_type="html">Reactive Halogens in the Marine Boundary Layer (RHaMBLe): the tropical North Atlantic experiments</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>J. D. Lee</name>
		</author>
		<author numeration="2" affiliations="3">
			<name>G. McFiggans</name>
		</author>
		<author numeration="3" affiliations="3,4">
			<name>J. D. Allan</name>
		</author>
		<author numeration="4" affiliations="5">
			<name>A. R. Baker</name>
		</author>
		<author numeration="5" affiliations="6">
			<name>S. M. Ball</name>
		</author>
		<author numeration="6" affiliations="7">
			<name>A. K. Benton</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>L. J. Carpenter</name>
		</author>
		<author numeration="8" affiliations="8">
			<name>R. Commane</name>
		</author>
		<author numeration="9" affiliations="9,20">
			<name>B. D. Finley</name>
		</author>
		<author numeration="10" affiliations="10">
			<name>M. Evans</name>
		</author>
		<author numeration="11" affiliations="3">
			<name>E. Fuentes</name>
		</author>
		<author numeration="12" affiliations="8,21">
			<name>K. Furneaux</name>
		</author>
		<author numeration="13" affiliations="8">
			<name>A. Goddard</name>
		</author>
		<author numeration="14" affiliations="3">
			<name>N. Good</name>
		</author>
		<author numeration="15" affiliations="1">
			<name>J. F. Hamilton</name>
		</author>
		<author numeration="16" affiliations="8,11">
			<name>D. E. Heard</name>
		</author>
		<author numeration="17" affiliations="12">
			<name>H. Herrmann</name>
		</author>
		<author numeration="18" affiliations="6">
			<name>A. Hollingsworth</name>
		</author>
		<author numeration="19" affiliations="1,2">
			<name>J. R. Hopkins</name>
		</author>
		<author numeration="20" affiliations="8,11">
			<name>T. Ingham</name>
		</author>
		<author numeration="21" affiliations="3">
			<name>M. Irwin</name>
		</author>
		<author numeration="22" affiliations="1">
			<name>C. E. Jones</name>
		</author>
		<author numeration="23" affiliations="7">
			<name>R. L. Jones</name>
		</author>
		<author numeration="24" affiliations="13">
			<name>W. C. Keene</name>
		</author>
		<author numeration="25" affiliations="9">
			<name>M. J. Lawler</name>
		</author>
		<author numeration="26" affiliations="12">
			<name>S. Lehmann</name>
		</author>
		<author numeration="27" affiliations="1,2">
			<name>A. C. Lewis</name>
		</author>
		<author numeration="28" affiliations="13">
			<name>M. S. Long</name>
		</author>
		<author numeration="29" affiliations="8">
			<name>A. Mahajan</name>
		</author>
		<author numeration="30" affiliations="14">
			<name>J. Methven</name>
		</author>
		<author numeration="31" affiliations="1">
			<name>S. J. Moller</name>
		</author>
		<author numeration="32" affiliations="12">
			<name>K. MÃ¼ller</name>
		</author>
		<author numeration="33" affiliations="12">
			<name>T. MÃ¼ller</name>
		</author>
		<author numeration="34" affiliations="12">
			<name>N. Niedermeier</name>
		</author>
		<author numeration="35" affiliations="15">
			<name>S. O&apos;Doherty</name>
		</author>
		<author numeration="36" affiliations="8">
			<name>H. Oetjen</name>
		</author>
		<author numeration="37" affiliations="8">
			<name>J. M. C. Plane</name>
		</author>
		<author numeration="38" affiliations="16,17">
			<name>A. A. P. Pszenny</name>
		</author>
		<author numeration="39" affiliations="1">
			<name>K. A. Read</name>
		</author>
		<author numeration="40" affiliations="18">
			<name>A. Saiz-Lopez</name>
		</author>
		<author numeration="41" affiliations="9">
			<name>E. S. Saltzman</name>
		</author>
		<author numeration="42" affiliations="19">
			<name>R. Sander</name>
		</author>
		<author numeration="43" affiliations="5">
			<name>R. von Glasow</name>
		</author>
		<author numeration="44" affiliations="8,11">
			<name>L. Whalley</name>
		</author>
		<author numeration="45" affiliations="12">
			<name>A. Wiedensohler</name>
		</author>
		<author numeration="46" affiliations="15">
			<name>D. Young</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry, University of York, Heslington, York, YO10 5DD, UK</affiliation>
		<affiliation numeration="2" content_type="html">National Centre for Atmospheric Sciences, University of York, Heslington, York, YO10 5DD, UK</affiliation>
		<affiliation numeration="3" content_type="html">Centre for Atmospheric Sciences, School of Earth, Atmospheric &amp; Environmental Sciences, University of Manchester, Manchester, M13 9PL, UK</affiliation>
		<affiliation numeration="4" content_type="html">National Centre for Atmospheric Sciences, University of Manchester, Manchester, M13 9PL, UK</affiliation>
		<affiliation numeration="5" content_type="html">School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK</affiliation>
		<affiliation numeration="6" content_type="html">Department of Chemistry, University of Leicester, Leicester, LE1 7RH, UK</affiliation>
		<affiliation numeration="7" content_type="html">Department of Chemistry, University of Cambridge, Lensfield Road, Cambridge, CB2 1EW, UK</affiliation>
		<affiliation numeration="8" content_type="html">School of Chemistry, University of Leeds, Leeds, LS2 9JT, UK</affiliation>
		<affiliation numeration="9" content_type="html">School of Physical Sciences, University of California, Irvine, CA 92697, USA</affiliation>
		<affiliation numeration="10" content_type="html">Institute for Atmospheric Science, School of Earth and the Environment, University of Leeds, LS2 9JT, UK</affiliation>
		<affiliation numeration="11" content_type="html">National Centre for Atmospheric Sciences, University of Leeds, Leeds, LS2 9JT, UK</affiliation>
		<affiliation numeration="12" content_type="html">Leibniz Institute for Tropospheric Research, PermoserstraÃŸe 15, 04318, Leipzig, Germany</affiliation>
		<affiliation numeration="13" content_type="html">Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA</affiliation>
		<affiliation numeration="14" content_type="html">Department of Meteorology, University of Reading, P.O. Box 243, Earley Gate, Reading, RG6 6BB, UK</affiliation>
		<affiliation numeration="15" content_type="html">School of Chemistry, University of Bristol, Bristol, BS8 1TS, UK</affiliation>
		<affiliation numeration="16" content_type="html">Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH 03824, USA</affiliation>
		<affiliation numeration="17" content_type="html">Mount Washington Observatory, North Conway, NH 03860, USA</affiliation>
		<affiliation numeration="18" content_type="html">NASA Jet propulsion Laboratory, California Institute of Technology, Pasadena, 91109, USA</affiliation>
		<affiliation numeration="19" content_type="html">Department of Atmospheric Chemistry, Max-Planck Institute of Chemistry, 55020 Mainz, Germany</affiliation>
		<affiliation numeration="20" content_type="html">now at: Program in Science and Technology, Univ. of Washington, Bothell, WA 98011, USA</affiliation>
		<affiliation numeration="21" content_type="html">sadly passed away, 28 July 2009</affiliation>
	</affiliations>
	<abstract content_type="html">The NERC UK SOLAS-funded Reactive Halogens in the Marine
Boundary Layer (RHaMBLe) programme comprised three field
experiments. This manuscript presents an overview of the
measurements made within the two simultaneous remote
experiments conducted in the tropical North Atlantic in May
and June 2007. Measurements were made from two mobile and one
ground-based platforms. The heavily instrumented cruise D319
on the RRS Discovery from Lisbon, Portugal to SÃ£o Vicente,
Cape Verde and back to Falmouth, UK was used to characterise
the spatial distribution of boundary layer components likely
to play a role in reactive halogen chemistry. Measurements
onboard the ARSF Dornier aircraft were used to allow the
observations to be interpreted in the context of their
vertical distribution and to confirm the interpretation of
atmospheric structure in the vicinity of the Cape Verde
islands. Long-term ground-based measurements at the Cape Verde
Atmospheric Observatory (CVAO) on SÃ£o Vicente were
supplemented by long-term measurements of reactive halogen
species and characterisation of additional trace gas and
aerosol species during the intensive experimental period.
&lt;br&gt;&lt;br&gt;
This paper presents a summary of the measurements made within
the RHaMBLe remote experiments and discusses them in their
meteorological and chemical context as determined from these
three platforms and from additional meteorological
analyses. Air always arrived at the CVAO from the North East
with a range of air mass origins (European, Atlantic and North
American continental). Trace gases were present at stable and
fairly low concentrations with the exception of a slight
increase in some anthropogenic components in air of North
American origin, though NO&lt;sub&gt;x&lt;/sub&gt; mixing ratios during this
period remained below 20 pptv. Consistency with these
air mass classifications is observed in the time series of
soluble gas and aerosol composition measurements, with
additional identification of periods of slightly elevated dust
concentrations consistent with the trajectories passing over
the African continent. The CVAO is shown to be broadly
representative of the wider North Atlantic marine boundary
layer; measurements of NO, O&lt;sub&gt;3&lt;/sub&gt; and black carbon
from the ship are consistent with a clean Northern Hemisphere
marine background. Aerosol composition measurements do not
indicate elevated organic material associated with clean
marine air.  Closer to the African coast, black carbon and
NO levels start to increase, indicating greater
anthropogenic influence.  Lower ozone in this region is
possibly associated with the increased levels of measured
halocarbons, associated with the nutrient rich waters of the
Mauritanian upwelling.  Bromide and chloride deficits in
coarse mode aerosol at both the CVAO and on D319 and the
continuous abundance of inorganic gaseous halogen species at
CVAO indicate significant reactive cycling of halogens.
&lt;br&gt;&lt;br&gt;
Aircraft measurements of O&lt;sub&gt;3&lt;/sub&gt; and CO show that
surface measurements are representative of the entire boundary
layer in the vicinity both in diurnal variability and absolute
levels.  Above the inversion layer similar diurnal behaviour
in O&lt;sub&gt;3&lt;/sub&gt; and CO is observed at lower mixing ratios
in the air that had originated from south of Cape Verde,
possibly from within the ITCZ. ECMWF calculations on two days
indicate very different boundary layer depths and aircraft
flights over the ship replicate this, giving confidence in the
calculated boundary layer depth.</abstract>
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