Major pathways of contaminants into and within the Arctic environment

A multi-compartment schematic diagram of the major pathways of contaminants into and within the Arctic environment
Major pathways of contaminants into and within the Arctic environment

Transport of 90Sr, originating from Sellafield, along the coast of Norway The highest values are found in the Norwegian Coastal Current and decrease northward

Transport of 90Sr, originating from Sellafield, along the coast of Norway The highest values are found in the Norwegian Coastal Current and decrease northward
Transport of 90Sr, originating from Sellafield, along the coast of Norway The highest values are found in the Norwegian Coastal Current and decrease northward

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

Annual radiation doses to critical groups from the Loviisa and Olkiluoto NPP’s

Annual radiation doses to critical groups from the Loviisa and Olkiluoto NPP’s
Annual radiation doses to critical groups from the Loviisa and Olkiluoto NPP’s

Collective doses from the Loviisa and Olkiluoto NPP’s

Collective doses from the Loviisa and Olkiluoto NPP’s
Collective doses from the Loviisa and Olkiluoto NPP’s

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

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

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

Comparison of doses to critical groups for Sellafield discharges from 1952 to 1993

Comparison of doses to critical groups for Sellafield discharges from 1952 to 1993
Comparison of doses to critical groups for Sellafield discharges from 1952 to 1993

Collective dose rates from European nuclear fuel reprocessing plants based on releases up to 1986

Collective dose rates from European nuclear fuel reprocessing plants based on releases up to 1986
Collective dose rates from European nuclear fuel reprocessing plants based on releases up to 1986

Collective dose commitment from nuclear fuel reprocessing activities

Collective dose commitment from nuclear fuel reprocessing activities
Collective dose commitment from nuclear fuel reprocessing activities

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



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