Search Results: "Atmospheric environment" OR "acidification" OR "air/aerosol" OR "sulphur and Sox"

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The time series of light scattering (?sp) and optical depth (?) at 500 nm at Barrow, Alaska The time series of light scattering (?sp) and optical depth (?) at 500 nm at Barrow, Alaska
Arctic surface air temperature Mean January and July surface air temperatures (°C) in the Arctic
Arctic sea-level atmospheric pressure (January) Mean atmospheric sea-level pressure (mb) in the Arctic in January
Nickel deposition to snow on the Kola Peninsula in April 1990 Nickel deposition to snow on the Kola Peninsula in April 1990
Changes with time in 131I activity concentration in Finnish air samples Changes with time in 131I activity concentration in Finnish air samples
Changes with time in 137Cs activity concentration in air in Norway, Finland and Russia Changes with time in 137Cs activity concentration in air in Norway, Finland and Russia
Changes with time in wet and dry deposition of 137Cs in Arctic Finland and north west Russia (Nenets Autonomous Okrug) Changes with time in wet and dry deposition of 137Cs in Arctic Finland and north west Russia (Nenets Autonomous Okrug)
Changes with time in wet and dry deposition of 90Sr in Arctic Finland and Greenland Changes with time in wet and dry deposition of 90Sr in Arctic Finland and Greenland
Locations of upper-air meteorological monitoring stations in the Arctic Meteorological station density for surface observations is greater for inland areas of the Arctic, while observations of any kind are sparse over the Arctic Ocean Locations of upper-air meteorological monitoring stations in the Arctic Meteorological station density for surface observations is greater for inland areas of the Arctic, while observations of any [..]
Lower tropospheric temperatures since 1979, from satellite monitoring High variability is characteristic of the Arctic region due to its isolation from the moderating influences of warm, lower latitude, ocean currents Lower tropospheric temperatures since 1979, from satellite monitoring High variability is characteristic of the Arctic region due to its isolation from the moderating influences of warm, lower [..]
Lower stratospheric (ca 120-40 hPa) Arctic temperature trends (°C per decade, January 1979 to February 1996), as monitored by MSUs on polar orbiting satellites Lower stratospheric (ca 120-40 hPa) Arctic temperature trends (°C per decade, January 1979 to February 1996), as monitored by MSUs on polar orbiting satellites
Lower tropospheric Arctic temperature trends (°C per decade, January 1979 to February 1996), as monitored by MSUs on polar orbiting satellites Lower tropospheric Arctic temperature trends (°C per decade, January 1979 to February 1996), as monitored by MSUs on polar orbiting satellites
Anthropogenic SO2 emissions for 1985 north of 30°N Anthropogenic SO2 emissions for 1985 north of 30°N
(a) The contribution from the different sources to the total deposition, averaged over the area north of 75°N from October 1990 to May 1994, (b) the calculated total monthly depositions of SOx averaged over the area north of 75°N, and (c) the (a) The contribution from the different sources to the total deposition, averaged over the area north of 75°N from October 1990 to May 1994, (b) the calculated total monthly depositions of SOx [..]
Model calculations of total (wet and dry) deposition estimates of sulfur for 1988 Model calculations of total (wet and dry) deposition estimates of sulfur for 1988

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