Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling pre 1960

Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling pre 1960
Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling pre 1960

Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1960 to 1979

Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1960 to 1979
Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1960 to 1979

Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1980 to 1989

Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1980 to 1989
Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1980 to 1989

Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1990 to 2004

Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1990 to 2004
Expansion of exploration drilling activity in arctic oil and gas provinces. Locations of drilling 1990 to 2004

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

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

Concentrations of sum-PCB, sum-HCH, and sum-DDT in seawater, ice, and overlying snow collected at approximately the same locations in the Russian Arctic in 1993-95

Concentrations of sum-PCB, sum-HCH, and sum-DDT in seawater, ice, and overlying snow collected at approximately the same locations in the Russian Arctic in 1993-95
Concentrations of sum-PCB, sum-HCH, and sum-DDT in seawater, ice, and overlying snow collected at approximately the same locations in the Russian Arctic in 1993-95

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

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

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

GDP in Arctic regions compared with national averages

GDP in Arctic regions compared with national averages (2002), showing the contribution of oil and gas extraction and pipeline transport to the regional GDP
GDP in Arctic regions compared with national averages

Main sources of icebergs and common iceberg drift trajectories The main ice circulation pattern follows the Transpolar Drift in the eastern Arctic and the Beaufort Gyre in the western Arctic (white arrows)

Main sources of icebergs and common iceberg drift trajectories The main ice circulation pattern follows the Transpolar Drift in the eastern Arctic and the Beaufort Gyre in the western Arctic (white [..]
Main sources of icebergs and common iceberg drift trajectories The main ice circulation pattern follows the Transpolar Drift in the eastern Arctic and the Beaufort Gyre in the western Arctic (white arrows)

(a) Trajectories of five satellite-tracked buoys launched in Mackenzie Bay, Canada, and (b) results of 30-day trajectories of oil launched from five hypothetical spill locations in the Beaufort Sea

(a) Trajectories of five satellite-tracked buoys launched in Mackenzie Bay, Canada, and (b) results of 30-day trajectories of oil launched from five hypothetical spill locations in the Beaufort Sea
(a) Trajectories of five satellite-tracked buoys launched in Mackenzie Bay, Canada, and (b) results of 30-day trajectories of oil launched from five hypothetical spill locations in the Beaufort Sea

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

Model evaluation comparing a five-day model simulation with results of an oil release experiment in the marginal ice zone near Svalbard in April 1993

Model evaluation comparing a five-day model simulation with results of an oil release experiment in the marginal ice zone near Svalbard in April 1993
Model evaluation comparing a five-day model simulation with results of an oil release experiment in the marginal ice zone near Svalbard in April 1993



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