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Climate and weather of the Australian Alps

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CLIMATEAND WEATHERThe<strong>wea<strong>the</strong>r</strong> in<strong>the</strong> pastOver many millions <strong>of</strong> years, <strong>the</strong> climate <strong>of</strong> Australia has changed many times. Sixmillion years ago rainforest covered much <strong>of</strong> Australia, including <strong>the</strong> <strong>Alps</strong>. Three millionyears ago colder conditions with increased rainfall dominated. Vast cold, treeless plainsreplaced <strong>the</strong> rainforest vegetation <strong>and</strong> <strong>the</strong> alpine plants <strong>and</strong> animals started to colonise<strong>the</strong> area. In <strong>the</strong> last two million years <strong>the</strong> area was covered by ice several times. In <strong>the</strong>glacial periods, <strong>the</strong> species <strong>of</strong> plants <strong>and</strong> animals that could withst<strong>and</strong> <strong>the</strong> cold, spreadout over <strong>the</strong> l<strong>and</strong>. As <strong>the</strong>se periods ended, <strong>the</strong>se species retreated back to <strong>the</strong> only areawhere it was still cold – <strong>the</strong> <strong>Australian</strong> <strong>Alps</strong>. These plants <strong>and</strong> animals had special characteristics,which species today still demonstrate, to cope with <strong>the</strong> wide temperaturevariations. The last Ice Age ended only 10,000 years ago.<strong>Climate</strong>changeIncreases in temperatures around <strong>the</strong> world due to <strong>the</strong> greenhouse effect will have significantimpacts on <strong>the</strong> <strong>Australian</strong> <strong>Alps</strong>. The global average temperature has increasedby approximately 0.6 °C in <strong>the</strong> past 100 years <strong>and</strong> is predicted to continue to rise. Anaverage global warming <strong>of</strong> 0.7 to 2.5 °C is predicted by 2050 <strong>and</strong> 1.4 to 5.8 °C by 2100.<strong>Climate</strong> change may cause a dryer, hotter climate, less snow <strong>and</strong> more frequent <strong>and</strong> extremefire <strong>and</strong> <strong>wea<strong>the</strong>r</strong> events in <strong>the</strong> <strong>Australian</strong> <strong>Alps</strong>. Warmer temperatures that leng<strong>the</strong>nsummer, or result in warmer autumns <strong>and</strong> winters, mean less snow will fall. The bestcasescenario for snow is <strong>the</strong> least increase in temperature <strong>and</strong> <strong>the</strong> greatest increase inwinter precipitation. Even a modest warming <strong>of</strong> 0.6°C by 2050 will result in a reduction<strong>of</strong> 15 to 20 days <strong>of</strong> snow cover in <strong>the</strong> <strong>Australian</strong> <strong>Alps</strong>.The naturalGreenhouseEffect.Some <strong>of</strong> <strong>the</strong> sun’s radiationis reflected back into spaceby <strong>the</strong> atmosphere, clouds<strong>and</strong> <strong>the</strong> earth. 51% passesthrough <strong>the</strong> atmosphere <strong>and</strong>warms <strong>the</strong> earth’s surface.Some <strong>of</strong> this warmth escapesas infra-red radiation. Gasesin <strong>the</strong> atmosphere, like watervapour, Carbon Dioxide,Methane, Chlor<strong>of</strong>luorocarbons,Halons <strong>and</strong> NitrousOxide absorb <strong>and</strong> re-emitsome <strong>of</strong> <strong>the</strong> infra-red, effectivelywarming <strong>the</strong> loweratmosphere <strong>and</strong> earth byabout 35The enhancedGreenhouseEffect.An increase in <strong>the</strong>quantity <strong>of</strong> Greenhousegases as a result <strong>of</strong>human activity, mayincrease temperatures.EDUCATION RESOURCE CLIMATE AND WEATHER 4/7

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