Graphics
Digital Data
A.M. Brounshtein,* A.A. Shashkov, N.N. Paramonova,
V.I. Privalov, Y.A. Starodubtsev
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1983-90
Air is collected generally four times per month in pairs of 1.5-L stainless steel electropolished flasks with one greaseless stainless steel stopcock. Sampling is performed by opening the stopcock of the flasks, which have been evacuated at the central laboratory at the Main Geophysical Observatory (MGO). The air is not dried during sample collection. Attempts are made to obtain samples when the wind speed is >5 m/s and the wind direction corresponds to the predetermined "clean air" sector.
After the air samples are collected, the flasks are mailed to the central laboratory at the MGO once per month for CO2 determinations, which are made through the use of a URAS-2T nondispersive infrared gas analyzer. Storage times between sample collection and analysis range from 2 to 6 months. Air samples are dried cryogenically before analysis.
The URAS-2T nondispersive infrared gas analyzer is calibrated by using CO2-in-synthetic air reference gases. All gases were initially calibrated at the Scripps Institution of Oceanography (SIO) against the primary standards maintained by the World Meteorological Organization (WMO) and against NOAA/GMCC standards in 1981. In 1988 and 1989, MGO reference gases were compared with a NOAA/GMCC set of three travelling CO2-in-air gas standards. During 1990-93, 13 series of calibrations were performed against a set of 5 CO2-in-air-standards provided by the Atmospheric Environment Service (AES) of Canada. On the basis of these calibration experiments, all MGO data were recalculated to a new scale that is closely related to the WMO X87 scale through the AES standards. A 2-year field comparison program with AES, involving a regular exchange of air samples from Alert and Teriberka, showed that data from both programs are comparable within 0.2 parts per million (ppm).
Concentration values for both flasks in a pair are accepted if the difference between the values is <1 ppmv. More details about the sampling methods and selection criteria are provided in Brounshtein et al. (1985, 1988a, 1988b, 1988c) and in Shashkov and Paramonova (in press).
An open ocean site in the North Atlantic, east of Greenland, was
established in 1968 and was operated in cooperation with NOAA's
National Weather Service through 1973. The Main Geophysical
Observatory collected flask samples at the site from January 1983
through October 1990. The yearly mean atmospheric
CO concentration
at Station "C" rose from 348.15 parts per million by volume (ppmv)
in 1985 to 354.33 ppmv in 1989.
CITE AS: Brounshtein, A.M., A.A. Shashkov, N.N. Paramonova, V.I. Privalov, and Y.A. Starodubtsev. 1994. Atmospheric CO2 records from sites in the Main Geophysical Observatory air sampling network. In Trends: A Compendium of Data on Global Change. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn., U.S.A.
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