Where in Australia is a non zonal climate? The reason?

In the north-east of Australia, it should be hot grass, but it is actually hot rain. The cause is that there is more precipitation on the windward slope of the Great Dividing Range, and in terms of ocean currents, the East Australian warm current warms and warms.

Australia's climate is characterized by a northern savannah climate, a northeastern rainforest climate, and a southern savannah climate. Its climate is characterized by the fact that the central and western regions of Australia are uninhabited deserts, with drought and little rain, high temperatures and large temperature differences; In the coastal zone, rainfall is abundant and the climate is humid.

Australia is located in the southern hemisphere, and although the time difference is only 2-3 hours from China, the seasons are completely opposite. Summer is from December to February, autumn from March to May, winter from June to August, and spring from September to November. The average annual temperature is 27 in the north and 14 in the south.

The causes of Australia's climate.

1. The cause of the savannah climate in northern Australia is that the equatorial low pressure belt moves southward in summer, low pressure appears on the Australian continent, and the northeast trade winds in the northern hemisphere deflect into the northwest monsoon across the equator, which comes from the low-latitude ocean, forming rich precipitation, and entering the rainy season in winter: the subtropical high moves northward, the Australian continent is controlled by the subtropical high, and the north is controlled by the southeast trade wind belt, and the southeast trade winds come from the inland, with less precipitation, and enter the dry season.

2. The cause of the tropical rainforest climate in northeast Australia is the southeast trade winds from the ocean, which bring sufficient water vapor and form abundant precipitation under the uplift of the terrain. There is also the East Australian Warm Stream flowing along the coast, which warms and humidifies.

3. The cause of the savannah climate in southern Australia is controlled by the subtropical high and westerly wind belt, which belongs to the transitional type of tropical desert and Mediterranean climate, but due to the low latitude, the temperature is higher and the evaporation is stronger, forming a savannah landscape.

Australia straddles two climatic zones, with the northern part having a tropical climate. Southern Australia has a temperate climate with four distinct seasons. The Australian interior is a desert with drought and little rainfall, high temperatures and large temperature differences; On the contrary, in the coastal areas, there is abundant rainfall, and the climate is humid and has a distinctly oceanic nature.

In addition, Australia is located in the southern hemisphere, although the time difference with China (including Hong Kong, Macao and Taiwan) is only 2-3 hours, but the season is completely opposite. Summer is from December to February, autumn is from March to May, winter is from June to August, and spring is from September to November. So now we're just in the summer, and Australia is just in the winter.

Australia straddles two climatic zones, the northern part is tropical, the rainy season is from November to April of the following year, the dry season is from November to April of the following year, and the typhoon period is from January to February due to its proximity to the equator.

Yes. Australia straddles two climatic zones, tropical in the north and temperate in the south.

Australia's climate is dominated by tropics: tropical desert climate near the Tropic of Capricorn, savannah climate around it, tropical rainforest climate in the northeast, temperate oceanic climate and Mediterranean climate in the southeast corner, and Mediterranean climate in a small area in the southwest corner.

Tropical climate is predominantly tropical desert climate near the Tropic of Cancer, then the outer ring is the savannah, the northeast is the tropical rainforest climate, the southeast corner has a temperate ocean climate and a Mediterranean climate, and the southwest corner has a little Mediterranean climate.

It is distributed in a semi-circular shape.

Australia's climate is characterized by its arid or semi-arid climate, which is the driest continent in the world.

Most of Australia, about 70 percent of the country, is arid or semi-arid, with much of the central region uninhabitable. Australia has 11 large deserts, and they cover about 20 of the entire continent. Due to the low rainfall, more than one-third of the continent is actually covered by desert.

Australia is the flattest and driest continent in the world, with dry deserts in the central depression and western plateau.

The average annual rainfall in Australia is 465 mm, and the annual rainfall varies widely and unevenly. The driest region is the Lake Eyre basin, with an average annual rainfall of less than 125 mm. The wettest places are in the north-eastern tropics and south-west Tasmania.

The climate varies greatly across Australia. The northern part of the continent has a humid tropical climate, the east** region and the western coast have a warm and not too hot climate, while the south coast of the continent and Tasmania have cooler climates. Overall, there are warm summers and not-so-cold winters across Australia.

The warmest place on record in Australia was in the north-eastern interior of Crooncari, where temperatures reached as high as 53 in 1889; The coldest place is Charlotte Pass, where in 1994 the lowest temperature recorded in the snow near Mount Corciakos was minus 23. The northern part is tropical, and most of it is temperate. The average annual temperature is 27 in the north and 14 in the south, with drought and little rain in the inland areas, with an annual precipitation of less than 200 mm, and 504-1200 mm in the eastern mountains.

It is distributed in a semi-circular shape. Australia straddles two climatic zones, with the northern part being tropical, and due to its proximity to the equator, January-February is the typhoon season. Southern Australia is temperate.

The central and western regions of Australia are uninhabited deserts, with drought and little rainfall, high temperatures and large temperature differences; In the coastal zone, rainfall is abundant and the climate is humid.

Australia is a highly developed capitalist country with its capital in Canberra. As the most economically developed country in the southern hemisphere, the 12th largest economy in the world, the fourth largest exporter of agricultural products in the world, and the world's largest exporter of various minerals, it is also called "the country sitting on a minecart".

Minerals: Australia is rich in mineral resources, oil and natural gas, with at least 70 kinds of mineral resources. Among them, bauxite reserves rank first in the world, accounting for 35% of the world's total reserves. Australia is the world's largest producer of bauxite, alumina, diamonds, lead and tantalum.

Biology: Australia is known as the "Living Fossil Museum of the World". According to statistics, there are 10,000 species of plants in Australia, and there are 9,000 species that other countries do not have; There are 650 species of birds, 450 of which are endemic to Australia.

The majority of the world's marsupials, with the exception of South America, are found in Australia. Due to its stable environment, Australia is endemic to ancient species that have been preserved during the evolution of the earth.

The distribution of climate types in Australia is roughly annular and semi-circular.

Australia straddles two climatic zones, with the northern part having a tropical climate. Southern Australia has a temperate climate with four distinct seasons. The Australian interior is a desert with drought and little rainfall, high temperatures and large temperature differences; In the coastal areas, rainfall is abundant and the climate is humid and has a distinctly oceanic nature.