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Australia has a wide variety of climates due to its large geographical size. The largest part of Australia is desert or semi-arid. Only the south-east and south-west corners have a temperate climate and moderately fertile soil. The northern part of the country has a tropical climate, varying between grasslands and desert.
Exclusive economic zone. 8,148,250 km 2 (3,146,060 sq mi) The geography of Australia encompasses a wide variety of biogeographic regions being the world's smallest continent, while comprising the territory of the sixth-largest country in the world. The population of Australia is concentrated along the eastern and south-eastern coasts.
Climate of Australia. The Australian environment ranges from virtually pristine Antarctic territory and rainforests to degraded industrial areas of major cities. Forty distinct ecoregions have been identified across the Australian mainland and islands. Central Australia has a very dry climate.
Climate of Melbourne. Summer rain over Melbourne, taken from Brighton. Winter fog over the Melbourne city centre. Melbourne, the state capital of Victoria and the second most populous city in Australia (most populous in urban area), has a temperate oceanic climate (Köppen climate classification Cfb), [1][2] bordering on a humid subtropical ...
Climate classifications are systems that categorize the world's climates. A climate classification may correlate closely with a biome classification, as climate is a major influence on life in a region. One of the most used is the Köppen climate classification scheme first developed in 1884. [1]
A thunderstorm in Sydney. The climate of Sydney, Australia is humid subtropical (Köppen: Cfa), [1] shifting from mild [2] [3] [4] and cool [5] in winter to warm and occasionally hot [5] in the summer, with no extreme seasonal differences as the weather is moderated by proximity to the ocean, [3] although more contrasting temperatures are recorded in the inland western suburbs.
The Köppen climate classification divides climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are A (tropical), B (arid), C (temperate), D (continental), and E (polar). Each group and subgroup is represented by a letter.
The average daily maximum temperature in Adelaide for February 2007 was 32.9 °C (91.2 °F), making it the second hottest on record only behind February 1906. The month included 15 days above 33 °C (91.4 °F) and 8 above 37 °C (98.6 °F). The warmest day was the 17th with a temperature of 41.5 °C (106.7 °F).