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NAVEGACION ANTARTICA - Iho-ohi.net

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ANTARCTICA<br />

Enclosed by cold sea currents<br />

Antarctic seas present a simple pattern of<br />

oceanic circulation: clockwise<br />

Antarctic seas with coldest summers; air<br />

temperatures between 0 o & -4 o C<br />

Sea ice surrounds the continent and the<br />

fresh ice<br />

Old sea ice, of several years, commonly<br />

lacks pronounced patterns of pools and<br />

drainage<br />

Sea ice of minor consistence<br />

Presents the major stational variation of sea<br />

ice extension: above the 75% of covered<br />

surface<br />

ARTIC<br />

Affected by the Gulf calid current<br />

Three different patterns of oceanic<br />

circulation: clockwise, counterclockwise<br />

and meridional<br />

More calid summers, with significative air<br />

temperatures above de 0 o C<br />

Sea ice is surrounded by the continent and<br />

fresh ice<br />

Old sea ice, of several years, commonly<br />

shows consistence patterns of pools and<br />

drainage<br />

Sea ice harder<br />

Confined sea ice, without presenting such<br />

grate Antarctic stational variations of extent<br />

* Research *<br />

Technical-scientific knowledge of the region<br />

in general poor, limited to summer<br />

campaigns and activities<br />

In the past, predominant summer activities<br />

and annual settlements<br />

Today, annual intense activities of selected<br />

countries. The rest maintain past conditions<br />

Wide and exhaustive technical-scientific<br />

knowledge of the region, extended to the<br />

Antarctic, by several institutions and<br />

universities of the Norther Hemisphere<br />

In the past, all year long activities of the<br />

countries involved in the region<br />

Today, as in the past, with great intensity of<br />

investigations<br />

A11 - 4

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