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Late one night in September 1999, ZL, travelling the inland road between the
Station and West Light, encountered a distinct pocket of acrid air
accumulated in a low sheltered hollow along the road. ZL returned to the
Station to report to the Station manager, and both then travelled between
West Light and the west end of the island to investigate. Although air
having the very strong chemical smell could be found only in several low
points along the inland road, the smoky plume from the Thebaud platform was
clearly visible and extended across the western end of the island.
The atmosphere of the Scotian Shelf region is affected, to some degree, by
activity associated with the offshore energy industry. Exploration and
production installations, supply and seismic vessels, and helicopters
produce various air emissions, including:
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combustion
products from engine exhaust and flares
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aerosol from incomplete combustion and/or
physical-chemical reactions
-
volatile and semi-volatile organic compounds (VOCs)
from incomplete combustion and fugitive emissions
Some of the above emissions
(e.g. combustion products such as oxides of nitrogen) are greenhouse gases.
Although none has been reported, hydrogen sulfide (H2S)
gas, from "sour" well developments, is also a potential airshed pollutant.
While MSC's greenhouse gases
program on Sable Island addresses continental and global pollution sources
and impacts, the primary focus of the airshed
monitoring program is to measure and identify sources of ambient air
emissions in the Scotian Shelf region. The Sable Island site is one of ten
air monitoring installations in Nova Scotia which provide ambient air
quality indexes relevant to human health. Also, the data from Sable Island
improves the overall accuracy of air quality predictions, and helps in
identification of air quality concerns within the region and implementation
of management strategies to address those concerns.
The quality
of the air we breathe is dependent on the rate that pollutants are emitted
into the atmosphere and the ability of the atmosphere to disperse these
pollutants. The movement and dispersion of air pollutants is controlled by
wind, temperature, turbulence and the changes in these elements caused by
local topography and/or oceanography. To gain a better understanding of
possible sources and behaviours of pollutants, the interpretation of the
data is supported by basic meteorological measurements of parameters that
affect the transport and dispersion of emissions. Measurements collected at
the Sable Island Station in support of the airshed monitoring program are:
wind speed and direction; temperature; solar radiation; and relative
humidity. Atmospheric modelling, which relies on meteorological and
aerological data collected at Sable Island and other stations, enables
researchers to generate back-trajectories for air parcels, and provides a
tool for study of circulation of atmospheric pollutants. Thus, if the
airshed monitoring program on Sable Island detects a pollution event,
researchers would be able to generate a back-trajectory indicating an origin
of the polluted air.
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This plot,
generated back to June 5th shows the routes travelled by air parcels, west
to east across the North American continent, arriving at Sable Island on
June 9th. The red, blue and green lines show the tracks of air
at
three different pressure
levels, corresponding to different altitudes. The red line represents
air flows at approximately 3000 meters, the blue line shows air flows at
approximately 1500 meters, and the green line shows air flows closest to the
ground. These flows move across the continent, but also move up and
down due to topography, temperature
changes, and the movement of pressure patterns.
For
example,
the low level flow
represented by the green line was at a pressure of 925 millibars. This
corresponded to 100 meters above sea level at its
western start, but at 750 meters above sea level over Sable Island.
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