Locations of sea dumping of radioactive waste in the Russian Arctic

Locations of sea dumping of radioactive waste in the Russian Arctic
Locations of sea dumping of radioactive waste in the Russian Arctic

Sequence of oil-ice interaction including drops under the ice, new ice growth below the oil, oil appearing on the surface in the spring, wind herding of oil on melt pools, and the appearance of emulsified oil on top of the ice

Sequence of oil-ice interaction including drops under the ice, new ice growth below the oil, oil appearing on the surface in the spring, wind herding of oil on melt pools, and the appearance of [..]
Sequence of oil-ice interaction including drops under the ice, new ice growth below the oil, oil appearing on the surface in the spring, wind herding of oil on melt pools, and the appearance of emulsified oil on top of the ice

Surface ocean currents in the Arctic

Surface ocean currents in the Arctic
Surface ocean currents in the Arctic

Conceptual model of the coastal zone and marine environments showing the main subcompartments and contaminant transfers, and exchanges with the atmosphere

Conceptual model of the coastal zone and marine environments showing the main subcompartments and contaminant transfers, and exchanges with the atmosphere
Conceptual model of the coastal zone and marine environments showing the main subcompartments and contaminant transfers, and exchanges with the atmosphere

Advanced Very High Resolution Radiometer (AVHRR) satellite image (June 4, 1986) showing a color composite of the visible data band for the Mackenzie Delta River water overflowing the landfast ice can be seen as purple regions

Advanced Very High Resolution Radiometer (AVHRR) satellite image (June 4, 1986) showing a color composite of the visible data band for the Mackenzie Delta River water overflowing the landfast ice can [..]
Advanced Very High Resolution Radiometer (AVHRR) satellite image (June 4, 1986) showing a color composite of the visible data band for the Mackenzie Delta River water overflowing the landfast ice can be seen as purple regions

Sketch of main circulation pattern in a fjord

Sketch of main circulation pattern in a fjord
Sketch of main circulation pattern in a fjord

Illustration of water, sediment and nutrient cycling in estuaries Freshwater flows outward, transporting sediments, plankton and also contaminants Material that sinks into the inflowing seawater may be trapped in the estuary

Illustration of water, sediment and nutrient cycling in estuaries Freshwater flows outward, transporting sediments, plankton and also contaminants Material that sinks into the inflowing seawater may [..]
Illustration of water, sediment and nutrient cycling in estuaries Freshwater flows outward, transporting sediments, plankton and also contaminants Material that sinks into the inflowing seawater may be trapped in the estuary

Schematic diagrams of the Greenland Sea showing the surface circulation (above) and water mass structure at a section across the central gyre (below)

Schematic diagrams of the Greenland Sea showing the surface circulation (above) and water mass structure at a section across the central gyre (below)
Schematic diagrams of the Greenland Sea showing the surface circulation (above) and water mass structure at a section across the central gyre (below)

Major surface currents in the North Atlantic Ocean

Major surface currents in the North Atlantic Ocean
Major surface currents in the North Atlantic Ocean

Surface currents in Hudson Bay, Hudson Strait and Foxe Basin

Surface currents in Hudson Bay, Hudson Strait and Foxe Basin
Surface currents in Hudson Bay, Hudson Strait and Foxe Basin

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

Above: contours of the asymptotic probability of ice formed in the hatched region moving into different parts of the Arctic Basin Below: contours of the asymptotic probability of ice moving from different areas into the hatched region and melting

Above: contours of the asymptotic probability of ice formed in the hatched region moving into different parts of the Arctic Basin Below: contours of the asymptotic probability of ice moving from [..]
Above: contours of the asymptotic probability of ice formed in the hatched region moving into different parts of the Arctic Basin Below: contours of the asymptotic probability of ice moving from different areas into the hatched region and melting

The predominant currents in the Arctic Ocean and their major routes around the basin edges of the Arctic

The predominant currents in the Arctic Ocean and their major routes around the basin edges of the Arctic
The predominant currents in the Arctic Ocean and their major routes around the basin edges of the Arctic

A schematic representation of the three-layer structure of the Arctic Ocean, with the Arctic Surface Layer above the Atlantic Water and Arctic Deep Water The residence time for the different water masses are also shown

A schematic representation of the three-layer structure of the Arctic Ocean, with the Arctic Surface Layer above the Atlantic Water and Arctic Deep Water The residence time for the different water [..]
A schematic representation of the three-layer structure of the Arctic Ocean, with the Arctic Surface Layer above the Atlantic Water and Arctic Deep Water The residence time for the different water masses are also shown

Surface currents in the Arctic region Square boxes indicate that the denser inflowing (Atlantic and Pacific) waters are submerging under the Polar Surface Water The continuation of these flows can be seen in Figure a03-27

Surface currents in the Arctic region Square boxes indicate that the denser inflowing (Atlantic and Pacific) waters are submerging under the Polar Surface Water The continuation of these flows can be [..]
Surface currents in the Arctic region Square boxes indicate that the denser inflowing (Atlantic and Pacific) waters are submerging under the Polar Surface Water The continuation of these flows can be seen in Figure a03-27



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