Search Results: "Arctic" OR "oil" OR "gas"

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SO2 emissions north of 50°N (modified after Benkovitz et al 1995, see Figure 91) showing point source emissions from Arctic and subarctic non-ferrous smelters and including natural DMS sources from the North Atlantic Ocean Area sources are not included SO2 emissions north of 50°N (modified after Benkovitz et al 1995, see Figure 91) showing point source emissions from Arctic and subarctic non-ferrous smelters and including natural DMS sources from [..]
The relative contribution to the 137Cs content of the diet of the ‘selected’ population of various Arctic areas for the period 1990 to 1994 The relative contribution to the 137Cs content of the diet of the ‘selected’ population of various Arctic areas for the period 1990 to 1994
Temporal variation in calculated reindeer Tag values for different Arctic regions Temporal variation in calculated reindeer Tag values for different Arctic regions
Spatial trends in the net flux from reindeer meat in different Arctic areas, for the first year after an assumed uniform deposition of 100 kBq/m2 Spatial trends in the net flux from reindeer meat in different Arctic areas, for the first year after an assumed uniform deposition of 100 kBq/m2
Sensitivity of Arctic ecosystems to acid deposition Sensitivity of Arctic ecosystems to acid deposition
The predicted (1988) average surface air sulfate concentrations in the Arctic The predicted (1988) average surface air sulfate concentrations in the Arctic
The predicted (1988) average surface air sulfur dioxide concentrations in the Arctic The predicted (1988) average surface air sulfur dioxide concentrations in the Arctic
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
The relative contribution to the 137Cs content of the diet of the ‘average’ population of various Arctic areas for the period 1990 to 1994 The relative contribution to the 137Cs content of the diet of the ‘average’ population of various Arctic areas for the period 1990 to 1994
The hydrologic balance in the Arctic is highly dynamic on the seasonal time scale with large and rapid ice melts in the spring On land, this ice and snow melting results in large rapid floods and surges in rivers The hydrologic balance in the Arctic is highly dynamic on the seasonal time scale with large and rapid ice melts in the spring On land, this ice and snow melting results in large rapid floods and [..]
Yearly intake of 137Cs from various dietary components by the average population of Arctic Canada Yearly intake of 137Cs from various dietary components by the average population of Arctic Canada
Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Canada Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Canada
Changes with time in 137Cs activity concentrations (5-year means) in lichens in Arctic Finland, Greenland, and Russia Changes with time in 137Cs activity concentrations (5-year means) in lichens in Arctic Finland, Greenland, and Russia

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