HR: 1340h
AN: A53C-1348 [Abstracts]
TI: The role of atmospheric transport in controlling mercury concentrations in wet deposition over
the northeastern United States
AU: * Weiss-Penzias, P S
EM: pweiss@ucsc.edu
AF: University of California, Santa Cruz, 1156 High St., Santa CruzCA, CA 95064, United States
AU: * Weiss-Penzias, P S
EM: pweiss@ucsc.edu
AF: Frontier Geosciences Inc., 414 Pontius Ave N, Seattle, WA 98109, United States
AU: Prestbo, E M
EM: eprestbo@tekran.com
AF: Tekran Instrument Corporation, 330 Nantucket Blvd., Toronto, ON M1P2P4, Canada
AU: Pollman, C D
EM: CurtisP@frontiergeosciences.com
AF: Frontier Geosciences Inc., 414 Pontius Ave N, Seattle, WA 98109, United States
AB:
The regional influence of large coal-combustion mercury sources on mercury concentrations in wet deposition in
the northeastern United States is investigated. Mercury concentrations in weekly precipitation samples were
obtained from four National Atmospheric Deposition Program (NADP) sites: Millford, PA (PA72), Huntington, NY
(NY20), Bridgton, ME (ME02), and Freeport, ME (ME96). Mean volume weighted mercury concentration at PA72
from 2001-2006 stands out as being about 25% higher (7.6 ng/L) than the other sites which showed equivalent
mercury concentrations (6 ng/L). Much of increase in mercury concentration at PA72 appears to occur in the
spring months (March-May), when the volume-weighted mean concentration (10.0 ng/L) is nearly 60% higher than
what is observed for the sites in New England (~6.3 ng/L). We find that these differences are largely due to the
unique location of PA72 relative to the major northeast U.S. outflow pathway. The dependence of mercury
concentrations on transport pathway is quantitatively determined by calculating how much time each precipitating
air mass has spent in a pre-defined emissions region using ensembles of HYSPLIT back trajectories for the
years 2004-2005. By totaling the number of trajectory hours that have positions inside this source region over the
same period of time as a weekly mercury sample, a parameter called "trajectory residence time" is generated.
Our results indicate that during the spring at PA72, trajectory residence time can explain about 60% of the
variability in the weekly mercury concentration. This relationship is much weaker at sites further to the north and
east. A comparison of the transport pathways between the six highest and lowest mercury concentration weekly
samples at PA72 reveals important seasonal changes that have a strong influence over peak and baseline
mercury concentrations. Our results allow us to estimate over what spatial scales the origins of mercury sources
are most likely: winter is a mix of global and regional, spring is almost entirely regional, summer is a mix of
regional and local, and fall is almost all local. Spring and summer are when emissions from the coal-
combustion source area have the most influence on mercury in precipitation at PA72. Because of this, we find
that there is a significant downward trend in the spring and summer months (0.9 ng/L/year, P<0.001, N=6), while
the fall and winter months show no trend. This suggests that further emissions reductions during the spring and
summer would have a proportionally larger effect of lowering mercury in wet deposition at PA72 than emissions
reductions at other times of the year.
DE: 0305 Aerosols and particles (0345, 4801, 4906)
DE: 0345 Pollution: urban and regional (0305, 0478, 4251)
DE: 0368 Troposphere: constituent transport and chemistry
DE: 0478 Pollution: urban, regional and global (0345, 4251)
DE: 4251 Marine pollution (0345, 0478)
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting