HR: 0800h
AN: A51C-0791 [Abstracts]
TI: Anthropogenic Emissions of Non-Methane Hydrocarbons in the Northeastern U.S.: 10 Years of Measured
Seasonal and Interannual Variations
AU: * Lee, H K
EM: lagoseco@berkeley.edu
AF: Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA
94720-3110
United States
AU: Munger, W J
EM: jwm@io.harvard.edu
AF: Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138
United States
AU: Wofsy, S C
EM: scw@io.harvard.edu
AF: Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138
United States
AU: Goldstein, A H
EM: ahg@nature.berkeley.edu
AF: Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA
94720-3110
United States
AB:
Harvard Forest, a rural site in central Massachusetts located downwind of major urban-industrial centers, provides an
excellent location to monitor anthropogenically emitted trace gases. Air that arrives at Harvard Forest from the southwest is
affected by emissions from the east-coast urban corridor, and may have residual influence from emissions in the upper Ohio
Valley and Great Lakes region further to the west. Pollution plumes that reach the site represent a homogenized mixture of
regional anthropogenic emissions. Concentrations of C$_{2}$-C$_{6}$ hydrocarbons along with CO, NO$_{y}$ and CH$_{4}$ were
measured nearly continuously from August 1992 through July 2002. By ratioing observed concentrations to acetylene, which is
almost solely produced from fossil-fuel combustion processes, we are able to detect seasonal and interannual trends in
relative emission rates for this series of trace gases. Furthermore, the variations in relative concentrations indicate
seasonal shifts in decomposition and deposition rates for shorter-lived compounds. Seasonal changes in butane and isobutane
emissions are dominated by changes in gasoline formulation that occur in the spring and fall transition. The seasonality of
pentane, isopentane and hexane emissions is dominated by temperature driven evaporative processes. Emissions of ethane and
propane lack seasonality and correlate less with acetylene than other gases, which indicate sources of these two gases are
strongly influenced by relatively local liquid propane, wood combustion and/or natural gas emissions that are not associated
with regional combustion sources. A strong seasonal shift in the CO to acetylene slope suggests that secondary production of
CO from oxidation of primary hydrocarbons in the summer significantly contributes to regional CO concentrations. The slope of
NO$_{y}$ to acetylene provides a better estimate of the fraction of NO$_{y}$ removed by deposition within the region during
summer than compared to the slope to CO.
DE: 0345 Pollution--urban and regional (0305)
SC: Atmospheric Sciences [A]
MN: 2004 AGU Fall Meeting