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Since Tasmania
lies between 40°S and 43.5°S and is an island with no place more than
115 kilometres from the sea, its climate is classified as temperate
maritime. On the coast the range of daily temperature is about 7°C,
but inland, the range is almost double, indicating a slight continental
effect.
Mountainous regions
cover a large proportion of Tasmania and attain a maximum height of
1617 metres at Mt Ossa, which rises from a central plateau. The central
plateau includes several peaks in excess of 1500 metres. A smaller mountainous
region in the northeast of Tasmania culminates with Ben Lomond, at an
elevation of 1573 metres.
Prevailing westerly
winds produce a marked west to east variation of cloudiness and rainfall,
but the variation of temperature is more governed by the elevation and
distance from the coast.
Summers are mild
and are characterised by greatly lengthened days. The sun reaches a
maximum elevation of 70 to 73 degrees in the midsummer, giving about
15 hours of daylight. In midwinter, the sun's elevation does not exceed
20 to 23 degrees, and the shortest day consists of about nine hours
of daylight.
In winter and early
spring, westerly winds reach their greatest strength and persistence
(they are also known as equinoctial gales) causing a distinct maximum
in the rainfall distribution in the west and northwest. In the east
and southeast, rainfall is more evenly distributed throughout the year.
In comparison with those areas of Europe and North America which are
at similar latitudes. Tasmania enjoys a very temperate climate. This
is due to the stabilising effect of surrounding oceans whose temperatures
change by some 6 or 7 degrees throughout the year. The higher proportion
of ocean to land area confers a similar benefit on the southern hemisphere
as a whole.
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