Backgo back Print current document
Resources / Maps & Graphics / Search Results


Your query returned 153 graphics.
Results 61 - 75

  Previous   1  2  3  4  5  6  7  8  9  10    Next  

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

A schematic diagram showing the inflow from the Mackenzie River trapped in the nearshore zone beneath the landfast ice Beyond the stamukhi zone, intermittent opening and refreezing in the flaw lead produces brine which encourages mixing and convection

A schematic diagram showing the inflow from the Mackenzie River trapped in the nearshore zone beneath the landfast ice Beyond the stamukhi zone, intermittent opening and refreezing in the flaw lead [..] 		A schematic diagram showing the inflow from the Mackenzie River trapped in the nearshore zone beneath the landfast ice Beyond the stamukhi zone, intermittent opening and refreezing in the flaw lead produces brine which encourages mixing and convection

Distribution of potential temperature, salinity, and density across the Arctic Ocean and the Greenland and Norwegian Seas

Distribution of potential temperature, salinity, and density across the Arctic Ocean and the Greenland and Norwegian Seas 		Distribution of potential temperature, salinity, and density across the Arctic Ocean and the Greenland and Norwegian Seas

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

Temperature and salinity of the Labrador Sea The cold freshwater from the Arctic Ocean and Baffin Bay is seen above the continental shelf

Temperature and salinity of the Labrador Sea The cold freshwater from the Arctic Ocean and Baffin Bay is seen above the continental shelf 		Temperature and salinity of the Labrador Sea The cold freshwater from the Arctic Ocean and Baffin Bay is seen above the continental shelf

Schematic diagram of circulation and the extent of different water masses in the Bering Sea

Schematic diagram of circulation and the extent of different water masses in the Bering Sea 		Schematic diagram of circulation and the extent of different water masses in the Bering Sea

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 [..] 		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)

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

Basic circulation and salinity distribution in salt wedge, partially-mixed, well-mixed and fjord-type estuaries as defined by Wollast and Duinker (1982) Numbers and shading show salinity values

Basic circulation and salinity distribution in salt wedge, partially-mixed, well-mixed and fjord-type estuaries as defined by Wollast and Duinker (1982) Numbers and shading show salinity values 		Basic circulation and salinity distribution in salt wedge, partially-mixed, well-mixed and fjord-type estuaries as defined by Wollast and Duinker (1982) Numbers and shading show salinity values

Sketch of main circulation pattern in a fjord

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

Surface ocean currents in the Arctic

Surface ocean currents in the Arctic 		Surface ocean currents in the Arctic
  Previous   1  2  3  4  5  6  7  8  9  10    Next  


To refine your search you can combine your search strings with AND, OR, NOT and NEAR and phrases can be quoted:
water OR waste searches for either of these words
oceans AND biodiversity searches for blocks with both words
pollution NEAR water searches for blocks with either of these words, with them being closer ranks higher
"climate change" searches for this phrase