Yearly intake of 137Cs from various dietary components by the average population of Arctic Russia

Yearly intake of 137Cs from various dietary components by the average population of Arctic Russia
Yearly intake of 137Cs from various dietary components by the average population of Arctic Russia

Yearly intake of 137Cs from various dietary components by the ‘selected’ population of eastern Arctic Russia

Yearly intake of 137Cs from various dietary components by the ‘selected’ population of eastern Arctic Russia
Yearly intake of 137Cs from various dietary components by the ‘selected’ population of eastern Arctic Russia

Yearly intake of 137Cs from various dietary components by the ‘selected’ population of western Arctic Russia

Yearly intake of 137Cs from various dietary components by the ‘selected’ population of western Arctic Russia
Yearly intake of 137Cs from various dietary components by the ‘selected’ population of western Arctic Russia

Yearly intake of 137Cs from various dietary components by the average population of Arctic Norway

Yearly intake of 137Cs from various dietary components by the average population of Arctic Norway
Yearly intake of 137Cs from various dietary components by the average population of Arctic Norway

Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Norway

Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Norway
Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Norway

Yearly intake of 137Cs from various dietary components by the average population of Arctic Sweden

Yearly intake of 137Cs from various dietary components by the average population of Arctic Sweden
Yearly intake of 137Cs from various dietary components by the average population of Arctic Sweden

Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Sweden

Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Sweden
Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Sweden

Integrated deposition density of 90Sr

Integrated deposition density of 90Sr
Integrated deposition density of 90Sr

Location of PUNE’s in Arctic Russia

Location of PUNE’s in Arctic Russia
Location of PUNE’s in Arctic Russia

Sites where atmospheric testing of nuclear weapons has taken place since 1945

Sites where atmospheric testing of nuclear weapons has taken place since 1945
Sites where atmospheric testing of nuclear weapons has taken place since 1945

The system of dams and drainage channels at Mayak

The system of dams and drainage channels at Mayak
The system of dams and drainage channels at Mayak

Mass transport pathways considered in the Coastal Zone Oil Spill Model (COZOIL), developed to simulate dynamic transport and weathering of oil on US Arctic coasts

Mass transport pathways considered in the Coastal Zone Oil Spill Model (COZOIL), developed to simulate dynamic transport and weathering of oil on US Arctic coasts
Mass transport pathways considered in the Coastal Zone Oil Spill Model (COZOIL), developed to simulate dynamic transport and weathering of oil on US Arctic coasts

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 cover

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 [..]
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 cover

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 [..]
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

Discharges of principle beta-gamma emitters in liquid effluent from Sellafield, 1952-1992

Discharges of principle beta-gamma emitters in liquid effluent from Sellafield, 1952-1992
Discharges of principle beta-gamma emitters in liquid effluent from Sellafield, 1952-1992



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