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An example of a positive feedback loop Warming leads to a decrease in sea ice cover which in turn leads to a decrease in albedo over the ocean, the result of which is further warming and further decreases in the sea ice coverAn example of a positive feedback loop Warming leads to a decrease in sea ice cover which in turn leads to a decrease in albedo over the ocean, the result of which is further warming and further [..] |
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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 riversThe 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 [..] |
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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 OceanLocations 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 [..] |
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Arctic boundaries (physical)The Arctic as defined by temperature, and the Arctic marine boundary, also showing the boundary of the AMAP assessment area |
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Arctic surface air temperatureMean January and July surface air temperatures (°C) in the Arctic |
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Model evaluation comparing a five-day model simulation with results of an oil release experiment in the marginal ice zone near Svalbard in April 1993Model evaluation comparing a five-day model simulation with results of an oil release experiment in the marginal ice zone near Svalbard in April 1993 |
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Schematic diagram of the Combined Model Ten climatic zones, each containing well-mixed compartments, are connected by meridional atmospheric and oceanic exchangeSchematic diagram of the Combined Model Ten climatic zones, each containing well-mixed compartments, are connected by meridional atmospheric and oceanic exchange |
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Temporal variation in calculated reindeer Tag values for different Arctic regionsTemporal variation in calculated reindeer Tag values for different Arctic regions |
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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/m2Spatial 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 |
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Temporal variation in cow milk Tag values for Sweden, Norway and FinlandTemporal variation in cow milk Tag values for Sweden, Norway and Finland |
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Comparison of the predicted flux of 137Cs in milk and reindeer meat in different Arctic areas, for the first year after an assumed uniform deposition of 100 kBq/m2Comparison of the predicted flux of 137Cs in milk and reindeer meat in different Arctic areas, for the first year after an assumed uniform deposition of 100 kBq/m2 |
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Norwegian counties considered in the flux vulnerability case studyNorwegian counties considered in the flux vulnerability case study |
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Relative 137Cs output in foodstuffs from the different Arctic Norwegian counties in the first year after an assumed uniform deposition of 100 kBq/m2Relative 137Cs output in foodstuffs from the different Arctic Norwegian counties in the first year after an assumed uniform deposition of 100 kBq/m2 |
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The comparative importance of different foodstuffs as sources of 137Cs for the three Arctic Norwegian counties over the 1-year and 50-year period following an assumed uniform deposition of 100 kBq/m2The comparative importance of different foodstuffs as sources of 137Cs for the three Arctic Norwegian counties over the 1-year and 50-year period following an assumed uniform deposition of 100 kBq/m2 |
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Distribution of the population of the three Arctic Norwegian countiesDistribution of the population of the three Arctic Norwegian counties |
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