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	<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>10</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-3347-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/3347/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/3347/2010/acpd-10-3347-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/3347/2010/acpd-10-3347-2010.pdf</fulltext_pdf>
	<start_page>3347</start_page>
	<end_page>3399</end_page>
	<publication_date>2010-02-09</publication_date>
	<article_title content_type="html">Long-range pollution transport during the MILAGRO-2006 campaign: a case study of a major Mexico City outflow event using free-floating altitude-controlled balloons</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. B. Voss</name>
			<email>pvoss@smith.edu</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>R. A. Zaveri</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>F. M. Flocke</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>H. Mao</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>T. P. Hartley</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>P. DeAmicis</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>I. Deonandan</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>G. Contreras-Jiménez</name>
		</author>
		<author numeration="9" affiliations="5">
			<name>O. Martínez-Antonio</name>
		</author>
		<author numeration="10" affiliations="6">
			<name>M. Figueroa Estrada</name>
		</author>
		<author numeration="11" affiliations="7">
			<name>D. Greenberg</name>
		</author>
		<author numeration="12" affiliations="3">
			<name>T. L. Campos</name>
		</author>
		<author numeration="13" affiliations="3">
			<name>A. J. Weinheimer</name>
		</author>
		<author numeration="14" affiliations="3">
			<name>D. J. Knapp</name>
		</author>
		<author numeration="15" affiliations="3">
			<name>D. D. Montzka</name>
		</author>
		<author numeration="16" affiliations="8">
			<name>J. D. Crounse</name>
		</author>
		<author numeration="17" affiliations="9,10">
			<name>P. O. Wennberg</name>
		</author>
		<author numeration="18" affiliations="3">
			<name>E. Apel</name>
		</author>
		<author numeration="19" affiliations="3">
			<name>S. Madronich</name>
		</author>
		<author numeration="20" affiliations="11">
			<name>B. de Foy</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Picker Engineering Program, Smith College, Northampton, MA, USA</affiliation>
		<affiliation numeration="2" content_type="html">Pacific Northwest National Laboratory, Richland, WA, USA</affiliation>
		<affiliation numeration="3" content_type="html">National Center for Atmospheric Research, Boulder, CO, USA</affiliation>
		<affiliation numeration="4" content_type="html">Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH, USA</affiliation>
		<affiliation numeration="5" content_type="html">Centro de Investigaciones Químicas, Universidad Autónoma del Estado de Morelos, Cuernavaca, Mexico</affiliation>
		<affiliation numeration="6" content_type="html">Instituto Nacional de Ecologia, Delegación Coyoacán, México D.F., Mexico</affiliation>
		<affiliation numeration="7" content_type="html">Mohawk Trail Regional School District, Shelburne Falls, MA, USA</affiliation>
		<affiliation numeration="8" content_type="html">Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA</affiliation>
		<affiliation numeration="9" content_type="html">Division of Engineering and Applied Science and Geological Science and Planetary Science, California Institute of Technology, Pasadena, CA, USA</affiliation>
		<affiliation numeration="10" content_type="html">Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA</affiliation>
		<affiliation numeration="11" content_type="html">Department of Earth and Atmospheric Sciences, Saint Louis University, St. Louis, MO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">One of the major objectives of the Megacities Initiative: Local And Global
Research Observations (MILAGRO-2006) campaign was to investigate the
long-range transport of polluted Mexico City Metropolitan Area (MCMA)
outflow and determine its downwind impacts on air quality and climate. Six
research aircraft, including the National Center for Atmospheric Research
(NCAR) C-130, made extensive chemical, aerosol, and radiation measurements
above MCMA and more than 1000 km downwind in order to characterize the
evolution of the outflow as it aged and dispersed over the Mesa Alta and
Gulf of Mexico. As part of this effort, free-floating
Controlled-Meteorological (CMET) balloons, commanded to change altitude via
satellite, made repeated profile measurements of winds and state variables
within the advecting outflow. In this paper, we present an analysis based on
the data from two CMET balloons that were launched near Mexico City on the
afternoon of 18 March 2006 and floated downwind with the MCMA pollution for
nearly 30 h. The repeating profile measurements show the evolving
structure of the outflow in considerable detail: its stability and
stratification, interaction with other air masses, mixing episodes, and
dispersion into the regional background. Air parcel trajectories, computed
directly from the balloon wind profiles, show three different transport
pathways on 18–19 March: (a) high-altitude advection of the top of the MCMA
mixed layer, (b) mid-level outflow over the Sierra Madre Oriental followed
by decoupling and isolated transport over the Gulf, and (c) low-altitude
outflow with entrainment into a cleaner westerly jet below the plateau. The
C-130 aircraft intercepted the balloon-based trajectories three times on
19 March, once along each of these pathways. In all three cases, distinct peaks
in the urban tracer signatures and LIDAR backscatter imagery were consistent
with MCMA pollution. The coherence of the high-altitude outflow was well
preserved after one day whereas that lower in the atmosphere was more widely
dispersed over the same time period. Other C-130 intercepts of polluted air
are shown to have likely originated outside of MCMA. These findings, and the
aircraft intercepts in particular, should prove useful in answering a range
of scientific questions pertaining to the transport, transformation, and
downwind impacts of megacity air pollution.</abstract>
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