Search Results: "Marine environment" OR "contaminant pathways" OR "radioactivity" OR "models"

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Illustration of the concept of a) the 'zone of influence' through major contaminant pathways from a major source region, and b) the 'contaminant focussing zone' resulting from the convergence of pathways carrying contaminants from a variety of sources Illustration of the concept of a) the 'zone of influence' through major contaminant pathways from a major source region, and b) the 'contaminant focussing zone' resulting from the convergence of [..]
Relationship between frequency and volume of releases to the marine environment from different sources (worldwide) Relationship between frequency and volume of releases to the marine environment from different sources (worldwide)
Geographical distribution of sample information in the AMAP radioactivity database Geographical distribution of sample information in the AMAP radioactivity database
Available data in the AMAP radioactivity database as a function of time Available data in the AMAP radioactivity database as a function of time
Ranges and average values of 137Cs activity concentrations in food products, from data in the AMAP radioactivity database Ranges and average values of 137Cs activity concentrations in food products, from data in the AMAP radioactivity database
A comparison of the structures of the Bergen, Toronto, and Combined zonally-averaged global models A comparison of the structures of the Bergen, Toronto, and Combined zonally-averaged global models
Distribution of radioactivity (PCi/L) in the surface layer of the ocean after ten years of simulation of Preller's model Source locations are the Ob, Yenisey and Pechora Rivers, as well as Sellafield Distribution of radioactivity (PCi/L) in the surface layer of the ocean after ten years of simulation of Preller's model Source locations are the Ob, Yenisey and Pechora Rivers, as well as Sellafield
Yearly and depth-averaged concentrations (Bq/m3) of 137Cs after 6 years from Harms' model The sources are instantaneous releases of 1 PBq from the dump sites in Abrosimov Bay, Stepovogo Bay, Tsivolky Bay, and Novaya Zemlya Trough Yearly and depth-averaged concentrations (Bq/m3) of 137Cs after 6 years from Harms' model The sources are instantaneous releases of 1 PBq from the dump sites in Abrosimov Bay, Stepovogo Bay, Tsivolky [..]
Vertically integrated tracer burden shown after 15 years Units are burden per unit surface area, normalized by cumulative release Bottom topography is in meters; a) no neptune, centered difference, and b) neptune, flux-corrected transport Vertically integrated tracer burden shown after 15 years Units are burden per unit surface area, normalized by cumulative release Bottom topography is in meters; a) no neptune, centered difference, [..]
Winter and summer surface water temperatures in the Arctic Ocean and adjacent seas Winter and summer surface water temperatures (°C) in the Arctic Ocean and adjacent seas
Winter and summer surface water salinity in the Arctic Ocean and adjacent seas Winter and summer surface water salinity in the Arctic Ocean and adjacent seas
The different domains of the Bering Sea continental shelf are separated by fronts The coastal domain (depth <50m) tends to be vertically homogeneous, the middle domain (50-100m) shows a clear two-layered structure, while the outer domain (100-170m) The different domains of the Bering Sea continental shelf are separated by fronts The coastal domain (depth <50m) tends to be vertically homogeneous, the middle domain (50-100m) shows a clear [..]
Circulation and water mass structure in the Arctic Ocean and Nordic Seas Mixing processes, such as brine formation, result in denser water that is transported off the shelves and into the deep basin Circulation and water mass structure in the Arctic Ocean and Nordic Seas Mixing processes, such as brine formation, result in denser water that is transported off the shelves and into the deep basin
Schematic representation of the temperature and salinity structure of the upper Arctic Ocean and how the halocline layer is maintained by brine-rich water produced on the shelves Schematic representation of the temperature and salinity structure of the upper Arctic Ocean and how the halocline layer is maintained by brine-rich water produced on the shelves
Schematic diagram of the Combined Model Ten climatic zones, each containing well-mixed compartments, are connected by meridional atmospheric and oceanic exchange Schematic 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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