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    16-May-2012
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Ice Features
West Coast of Svalbard
Vilkitskogo Strait
Southern Weddell Sea
South Orkney Island
Ronne Ice Shelf
Queen Maud Land
Icebergs off the East Greenland Coast
Odden ice tongue
Novaya Zemlya East Coast
Northernmost islands of the Siberian Coast
North-eastern Barents Sea
North Coast of Svalbard
New ice in the Kara Sea
Interior of the Arctic pack-ice
Icebergs off the East Greenland Coast
Ice movement in the Antarctica (Stereo)
Ice motion in Ob river estuary
Ice dynamics (Movie)
Ice dynamics inside the ice edge
Ice condition across the Denmark Strait
Ice-breaker route on Yenisei River
Ice-breaker navigation in Mathiessen Strait
Grounded icebergs
Glaciers of Franz Josef Land
From Greenland Coast towards Jan Mayen
Dynamics of the ice edge
Freeze-up in the Baydratskaya Bay
Fram Strait winter ice
First year and multiyear ice
Ekstroem Ice Shelf
Eddy currents in Pechora Sea
Dynamics of the ice edge
Deep sea drilling on the Yermark Plateau
Combined SAR and SSM/I data
Classification of winter ice
Changing ice edge in the Hopen area
"L'Astrolabe" expedition through the Northeast Passage
Antarctic Peninsula
SIZEX 92 experiment
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Vilkitskogo Strait

The Vilkitskogo Strait, which is the northernmost part of the Northeast Passage, is a very difficult area for ice navigation. Thick residual floes (second- or multiyear ice) often occur in this region where differential ice motion causes heavy compression and ridging of the ice pack. The large thick floes, heavy ridges and as well as landfast ice make it difficult to navigate even for the most powerful icebreakers. The ERS-1 SAR image of November 4, 1993 shows examples of the ice types which often occur in the Vilkitskogo Strait (see the location of the SAR image).

The "Sovetsky Soyuz" navigated along the Taimyr coast in the flaw lead denoted A, B, C. The polynya consisted of young ice 15-30 cm thick (dark signature) which was easy to penetrate. Other ice types are thin first-year ice about 40 cm thick (area D) and multiyear ice about 3 m thick. The multiyear ice has a high backscatter, in contrast to the young and first-year ice. Mapping of multiyear ice is very important because navigation through such ice is difficult and should be avoided. The SAR image of November 4 provided useful information for the icebreakers to find the best sailing route. Navigation through the flaw lead along the Taimyr coast was much faster and less difficult and hazardous than through alternative routes.

The Russian ice map (translated to English) of the same area is shown here.

NERSC, Bergen, Norway

Keywords: ESA European Space Agency - Agence spatiale europeenne, observation de la terre, earth observation, satellite remote sensing, teledetection, geophysique, altimetrie, radar, chimique atmospherique, geophysics, altimetry, radar, atmospheric chemistry