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Antarctic visits are mainly
concentrated at ice-free coastal zones over the Antarctic summer, the
five-month period from November to March, in high summer there will be 20+
hours of daylight. The formation and movement of sea-ice outside of
these times means that from March to November, Antarctica is left to
the over-wintering scientific bases and their crews. Tourist ships possibly
could get in and out earlier or later in the season, but there is the all
too real danger of not being able to get to the places on the itinerary, or
more importantly of being stuck in the sea-ice and having an enforced winter
(for an extra 8 months or more) as has happened on scientific bases
occasionally. Winter pack ice extends over 620 miles around the
continent, it is almost permanently dark and temperatures can drop to as low
as -90ºC (-130ºF)
Temperature Range; December - February 20ºF to 50ºF
-6ºC to +10ºC
November & Early
December (Late Spring / Early Summer)
Mid-December and
January (Mid Summer) February
and March (Late Summer) CLIMATE Antarctica is the coldest continent. The lowest
temperature ever recorded anywhere on earth, -88.3° C (-126.9° F), was on
August 24, 1960, at Vostok Station. The continent is also buffeted by heavy
winds. In the interior, winds as high as 320 km/h (200 mph) have been
recorded. These winds flow downslope from the interior toward the coast and,
combined with the low temperatures, create dangerous wind-chill conditions.
Three basic climatic regions can be distinguished
in Antarctica. The interior is characterized by extreme cold and light
snowfall; the coastal areas are characterized by somewhat milder
temperatures and much higher precipitation rates; and the Antarctic
Peninsula is characterized by a warmer and wetter climate, with
above-freezing temperatures common. Antarctica can be classified as a true desert; in
the interior the average annual precipitation (in water) is only about 50 mm
(about 2 in). Raging blizzards often occur, however, when winds pick up
previously deposited snow and move it from place to place. Annual
precipitation is much heavier along the coast, amounting to about 380 mm
(about 15 in) in water. Here, heavy snowfalls occur when cyclonic storms
pick up moisture from the surrounding seas; this moisture freezes and is
deposited as snow over the coastal areas. Along the Antarctic Peninsula, especially the
northern end, rain is as common as snow. The interior of Antarctica has
almost continuous daylight during the southern hemisphere's summer and
darkness during the southern hemisphere's winter. In coastal areas, which
are farther north, long periods of sunshine occur during the summer, but
sunrises and sunsets occur during much of the rest of the year. It's no exaggeration to call Antarctica the coldest,
windiest and driest place on Earth. The average continental temperature is
around -32 F/-36 C, and a few remote places-notably Adelie Land-get wind
gusts of up to 200 mph/322 kph. With only a few inches of precipitation a
year, Antarctica is technically the world's largest desert. In the Dry
Valley region, in fact, there is no snow or ice, giving the area a rocky,
lunar landscape. |
All rates in U.S. dollars. Prices,
savings offers, and other terms subject to change without notice.
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