R. A. Zaveri, Pacific Northwest National Laboratory
W. J. Shaw, Pacific Northwest National Laboratory
D. J. Cziczo, Massachusetts Institute of Technology
B. Schmid, Pacific Northwest National Laboratory
R. A. Ferrare, NASA Langley Research Center
M. L. Alexander, Environmental Molecular Sciences Laboratory
M. Alexandrov, Columbia University in the City of New York
R. J. Alvarez, National Oceanic and Atmospheric Administration
W. P. Arnott, University of Nevada, Reno
D. B. Atkinson, Portland State University
S. Baidar, University of Colorado Boulder
R. M. Banta, National Oceanic and Atmospheric Administration
J. C. Barnard, Pacific Northwest National Laboratory
J. Beranek, Pacific Northwest National Laboratory
L. K. Berg, Pacific Northwest National Laboratory
F. Brechtel, Brechtel Manufacturing Inc.
W. A. Brewer, National Oceanic and Atmospheric Administration
J. F. Cahill, University of California, San Diego
B. Cairns, NASA Goddard Institute for Space Studies
C. D. Cappa, University of California, Davis
D. Chand, Pacific Northwest National Laboratory
S. China, Michigan Technological UniversityFollow
J. M. Comstock, Pacific Northwest National Laboratory
M. K. Dubey, Los Alamos National Laboratory
R. C. Easter, Pacific Northwest National Laboratory
M. H. Erickson, Washington State University Pullman
J. D. Fast, Pacific Northwest National Laboratory
C. Floerchinger, Montana State University
B. A. Flowers, Los Alamos National Laboratory
E. Fortner, Aerodyne Research, Inc.
J. S. Gaffney, University of Arkansas at Little Rock
M. K. Gilles, Lawrence Berkeley National Laboratory

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Atmospheric Sciences


Substantial uncertainties still exist in the scientific understanding of the possible interactions between urban and natural (biogenic) emissions in the production and transformation of atmospheric aerosol and the resulting impact on climate change. The US Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) program's Carbonaceous Aerosol and Radiative Effects Study (CARES) carried out in June 2010 in Central Valley, California, was a comprehensive effort designed to improve this understanding. The primary objective of the field study was to investigate the evolution of secondary organic and black carbon aerosols and their climate-related properties in the Sacramento urban plume as it was routinely transported into the forested Sierra Nevada foothills area. Urban aerosols and trace gases experienced significant physical and chemical transformations as they mixed with the reactive biogenic hydrocarbons emitted from the forest. Two heavily-instrumented ground sites-one within the Sacramento urban area and another about 40 km to the northeast in the foothills area-were set up to characterize the evolution of meteorological variables, trace gases, aerosol precursors, aerosol size, composition, and climate-related properties in freshly polluted and "aged" urban air. On selected days, the DOE G-1 aircraft was deployed to make similar measurements upwind and across the evolving Sacramento plume in the morning and again in the afternoon. The NASA B-200 aircraft, carrying remote sensing instruments, was also deployed to characterize the vertical and horizontal distribution of aerosols and aerosol optical properties within and around the plume. This overview provides: (a) the scientific background and motivation for the study, (b) the operational and logistical information pertinent to the execution of the study, (c) an overview of key observations and initial findings from the aircraft and ground-based sampling platforms, and (d) a roadmap of planned data analyses and focused modeling efforts that will facilitate the integration of new knowledge into improved representations of key aerosol processes and properties in climate models.

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© 2012 Author(s). Publisher’s version of record:

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Atmospheric Chemistry and Physics

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