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  • Author or Editor: Allen H. Goldstein x
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Annmarie G. Carlton
,
Joost de Gouw
,
Jose L. Jimenez
,
Jesse L. Ambrose
,
Alexis R. Attwood
,
Steven Brown
,
Kirk R. Baker
,
Charles Brock
,
Ronald C. Cohen
,
Sylvia Edgerton
,
Caroline M. Farkas
,
Delphine Farmer
,
Allen H. Goldstein
,
Lynne Gratz
,
Alex Guenther
,
Sherri Hunt
,
Lyatt Jaeglé
,
Daniel A. Jaffe
,
John Mak
,
Crystal McClure
,
Athanasios Nenes
,
Thien Khoi Nguyen
,
Jeffrey R. Pierce
,
Suzane de Sa
,
Noelle E. Selin
,
Viral Shah
,
Stephanie Shaw
,
Paul B. Shepson
,
Shaojie Song
,
Jochen Stutz
,
Jason D. Surratt
,
Barbara J. Turpin
,
Carsten Warneke
,
Rebecca A. Washenfelder
,
Paul O. Wennberg
, and
Xianling Zhou

Abstract

The Southeast Atmosphere Studies (SAS), which included the Southern Oxidant and Aerosol Study (SOAS); the Southeast Nexus (SENEX) study; and the Nitrogen, Oxidants, Mercury and Aerosols: Distributions, Sources and Sinks (NOMADSS) study, was deployed in the field from 1 June to 15 July 2013 in the central and eastern United States, and it overlapped with and was complemented by the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys (SEAC4RS) campaign. SAS investigated atmospheric chemistry and the associated air quality and climate-relevant particle properties. Coordinated measurements from six ground sites, four aircraft, tall towers, balloon-borne sondes, existing surface networks, and satellites provide in situ and remotely sensed data on trace-gas composition, aerosol physicochemical properties, and local and synoptic meteorology. Selected SAS findings indicate 1) dramatically reduced NOx concentrations have altered ozone production regimes; 2) indicators of “biogenic” secondary organic aerosol (SOA), once considered part of the natural background, were positively correlated with one or more indicators of anthropogenic pollution; and 3) liquid water dramatically impacted particle scattering while biogenic SOA did not. SAS findings suggest that atmosphere–biosphere interactions modulate ambient pollutant concentrations through complex mechanisms and feedbacks not yet adequately captured in atmospheric models. The SAS dataset, now publicly available, is a powerful constraint to develop predictive capability that enhances model representation of the response and subsequent impacts of changes in atmospheric composition to changes in emissions, chemistry, and meteorology.

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Dennis Baldocchi
,
Eva Falge
,
Lianhong Gu
,
Richard Olson
,
David Hollinger
,
Steve Running
,
Peter Anthoni
,
Ch. Bernhofer
,
Kenneth Davis
,
Robert Evans
,
Jose Fuentes
,
Allen Goldstein
,
Gabriel Katul
,
Beverly Law
,
Xuhui Lee
,
Yadvinder Malhi
,
Tilden Meyers
,
William Munger
,
Walt Oechel
,
K. T. Paw U
,
Kim Pilegaard
,
H. P. Schmid
,
Riccardo Valentini
,
Shashi Verma
,
Timo Vesala
,
Kell Wilson
, and
Steve Wofsy

FLUXNET is a global network of micrometeorological flux measurement sites that measure the exchanges of carbon dioxide, water vapor, and energy between the biosphere and atmosphere. At present over 140 sites are operating on a long-term and continuous basis. Vegetation under study includes temperate conifer and broadleaved (deciduous and evergreen) forests, tropical and boreal forests, crops, grasslands, chaparral, wetlands, and tundra. Sites exist on five continents and their latitudinal distribution ranges from 70°N to 30°S.

FLUXNET has several primary functions. First, it provides infrastructure for compiling, archiving, and distributing carbon, water, and energy flux measurement, and meteorological, plant, and soil data to the science community. (Data and site information are available online at the FLUXNET Web site, http://www-eosdis.ornl.gov/FLUXNET/.) Second, the project supports calibration and flux intercomparison activities. This activity ensures that data from the regional networks are intercomparable. And third, FLUXNET supports the synthesis, discussion, and communication of ideas and data by supporting project scientists, workshops, and visiting scientists. The overarching goal is to provide information for validating computations of net primary productivity, evaporation, and energy absorption that are being generated by sensors mounted on the NASA Terra satellite.

Data being compiled by FLUXNET are being used to quantify and compare magnitudes and dynamics of annual ecosystem carbon and water balances, to quantify the response of stand-scale carbon dioxide and water vapor flux densities to controlling biotic and abiotic factors, and to validate a hierarchy of soil–plant–atmosphere trace gas exchange models. Findings so far include 1) net CO2 exchange of temperate broadleaved forests increases by about 5.7 g C m−2 day−1 for each additional day that the growing season is extended; 2) the sensitivity of net ecosystem CO2 exchange to sunlight doubles if the sky is cloudy rather than clear; 3) the spectrum of CO2 flux density exhibits peaks at timescales of days, weeks, and years, and a spectral gap exists at the month timescale; 4) the optimal temperature of net CO2 exchange varies with mean summer temperature; and 5) stand age affects carbon dioxide and water vapor flux densities.

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