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

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

Dose accumulation in adult rural residents after the Kyshtym accident in 1957

Dose accumulation in adult rural residents after the Kyshtym accident in 1957
Dose accumulation in adult rural residents after the Kyshtym accident in 1957

Photograph of a submarine being provided with cooling water from a supply ship

Photograph of a submarine being provided with cooling water from a supply ship
Photograph of a submarine being provided with cooling water from a supply ship

Dose estimates based on wholebody measurements (see Figure 836) for two groups (northern Saami and southern Saami) of Norwegian reindeer-breeding Saami

Dose estimates based on wholebody measurements (see Figure 836) for two groups (northern Saami and southern Saami) of Norwegian reindeer-breeding Saami
Dose estimates based on wholebody measurements (see Figure 836) for two groups (northern Saami and southern Saami) of Norwegian reindeer-breeding Saami

The changing inventory of major radionuclides in the Komsomolets reactor with time

The changing inventory of major radionuclides in the Komsomolets reactor with time
The changing inventory of major radionuclides in the Komsomolets reactor with time

Major Russian naval bases along the Kola Peninsula and White Sea

Major Russian naval bases along the Kola Peninsula and White Sea
Major Russian naval bases along the Kola Peninsula and White Sea

Tracer concentration on a vertical section (along Y=0 on Figure 346) after 15 years; a) no neptune, centered difference; b) neptune, flux-corrected transport; c,d) velocity normal to the section with positive "into" the page, negative "out" of the page;

Tracer concentration on a vertical section (along Y=0 on Figure 346) after 15 years; a) no neptune, centered difference; b) neptune, flux-corrected transport; c,d) velocity normal to the section with [..]
Tracer concentration on a vertical section (along Y=0 on Figure 346) after 15 years; a) no neptune, centered difference; b) neptune, flux-corrected transport; c,d) velocity normal to the section with positive "into" the page, negative "out" of the page;



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