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The Davis Strait - DCE - Nationalt Center for Miljø og Energi

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Figure 3.3.3. Average sea ice<br />

extent as percentage ice cover in<br />

West Greenland waters based on<br />

data in the period 1979-2007<br />

(medio March). Blue colours<br />

indicate highest percentage ice<br />

cover while red indicates lowest<br />

percentage cover. White has no<br />

data value. ’High’ ice cover is<br />

encountered west of Disko Island<br />

while low ice cover is found south<br />

of Sisimiut in March (Data<br />

sources: Ocean and Sea ice<br />

(EUMETSAT).<br />

75°N<br />

70°N<br />

70°W<br />

80°W<br />

Average sea ice extent<br />

(medio march 1979-2007)<br />

65°N<br />

Percent ice cover<br />

0 - 3<br />

4 - 13<br />

14 - 29<br />

30 - 45<br />

46 - 61<br />

62 - 77<br />

78 - 88<br />

89 - 94<br />

95 - 100<br />

Assessment area<br />

0 150 300 Km<br />

60°N<br />

70°W<br />

<strong>The</strong> process of calving from the front of a glacier produces an infinite variety<br />

of icebergs, bergy bits and growlers. Icebergs are described by their size according<br />

to the following classification:<br />

Type Height (m, above sea level) Length (m)<br />

growler less than 1 up to 5<br />

bergy bit 1 to 5 5 to 15<br />

small iceberg 5 to 15 15 to 60<br />

medium iceberg 16 to 45 61 to 120<br />

large iceberg 46 to 75 121 to 200<br />

very large iceberg Over 75 Over 200<br />

<strong>The</strong> production of icebergs on a volumetric basis varies only slightly from<br />

year to year. Once calving has been accomplished, meteorol<strong>og</strong>ical and<br />

ocean<strong>og</strong>raphic factors begin to affect the icebergs. Icebergs are carried by sea<br />

currents directed by the integrated average of the water motion over the<br />

60°W<br />

60°W<br />

50°W<br />

50°W<br />

40°W<br />

75°N<br />

70°N<br />

65°N<br />

59

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