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Innisfail, Queensland, Australia
Innisfail (from Irish: Inis Fáil) is a regional town and locality in the Cassowary Coast Region, Queensland, Australia. The town was originally called Geraldton until 1910. In the , the town of Innisfail had a population of 7,236 people, while the locality of Innisfail had a population of 1,145 people. Innisfail is the major township of the Cassowary Coast Region and is known for its sugar and banana industries, as well as for being one of Australia's wettest towns. In March 2006, Innisfail gained worldwide attention when severe Tropical Cyclone Larry passed over causing extensive damage. Geography Innisfail's town centre is situated at the junction of the Johnstone River and South Johnstone River, approximately from the coast. It is located near large tracts of old-growth tropical rainforest surrounded by vast areas of extensive farmlands. Queensland's highest mountain, Mount Bartle Frere; part of Australia's Great Dividing Range, is to the north. The town's c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
AEST
Australia uses three main time zones: Australian Western Standard Time (AWST; UTC+08:00), Australian Central Standard Time (ACST; UTC+09:30), and Australian Eastern Standard Time (AEST; UTC+10:00). Time is regulated by the individual state governments, some of which observe daylight saving time (DST). Australia's external territories observe different time zones. Standard time was introduced in the 1890s when all of the Australian colonies adopted it. Before the switch to standard time zones, each local city or town was free to determine its local time, called local mean time. Now, Western Australia uses Western Standard Time; South Australia and the Northern Territory use Central Standard Time; while New South Wales, Queensland, Tasmania, Victoria (Australia), Victoria, Jervis Bay Territory, and the Australian Capital Territory use Eastern Standard Time. Daylight saving time (+1 hour) is used in jurisdictions in the south and south-east: South Australia, New South Wales, Vict ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sugar
Sugar is the generic name for sweet-tasting, soluble carbohydrates, many of which are used in food. Simple sugars, also called monosaccharides, include glucose, fructose, and galactose. Compound sugars, also called disaccharides or double sugars, are molecules made of two bonded monosaccharides; common examples are sucrose (glucose + fructose), lactose (glucose + galactose), and maltose (two molecules of glucose). White sugar is a refined form of sucrose. In the body, compound sugars are hydrolysed into simple sugars. Longer chains of monosaccharides (>2) are not regarded as sugars, and are called oligosaccharides or polysaccharides. Starch is a glucose polymer found in plants, the most abundant source of energy in human food. Some other chemical substances, such as glycerol and sugar alcohols, may have a sweet taste, but are not classified as sugar. Sugars are found in the tissues of most plants. Honey and fruits are abundant natural sources of simple sugars. Suc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humid
Humidity is the concentration of water vapor present in the air. Water vapor, the gaseous state of water, is generally invisible to the human eye. Humidity indicates the likelihood for precipitation, dew, or fog to be present. Humidity depends on the temperature and pressure of the system of interest. The same amount of water vapor results in higher relative humidity in cool air than warm air. A related parameter is the dew point. The amount of water vapor needed to achieve saturation increases as the temperature increases. As the temperature of a parcel of air decreases it will eventually reach the saturation point without adding or losing water mass. The amount of water vapor contained within a parcel of air can vary significantly. For example, a parcel of air near saturation may contain 28 g of water per cubic metre of air at , but only 8 g of water per cubic metre of air at . Three primary measurements of humidity are widely employed: absolute, relative, and specific. Abs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone
In meteorology, a cyclone () is a large air mass that rotates around a strong center of low atmospheric pressure, counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as viewed from above (opposite to an anticyclone). Cyclones are characterized by inward-spiraling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale (the synoptic scale). Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes, and dust devils lie within smaller mesoscale. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. Cyclogenesis is the process of cyclone formation and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. 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. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropical Rainforest Climate
A tropical rainforest climate, humid tropical climate or equatorial climate is a tropical climate sub-type usually found within 10 to 15 degrees latitude of the equator. There are some other areas at higher latitudes, such as the coast of southeast Florida, USA, and Okinawa, Japan that fall into the tropical rainforest climate category. They experience high mean annual temperatures, small temperature ranges, and rain that falls throughout the year. Regions with this climate are typically designated ''Af'' by the Köppen climate classification. A tropical rainforest climate is typically hot, very humid, and wet. Description Tropical rain forests have a type of tropical climate in which there is no dry season—all months have an average precipitation value of at least . There are no distinct wet or dry seasons as rainfall is high throughout the months. One day in a tropical rainforest climate can be very similar to the next, while the change in temperature between day and night ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Innisfail Floods1
Innisfail may refer to: * Innisfail, Queensland, a town in the Cassowary Coast Region, Australia * Innisfail, Alberta, town in Canada * Inisfail, poetic name for Ireland See also * Innisfil, town in Ontario, Canada {{Disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Dividing Range
The Great Dividing Range, also known as the East Australian Cordillera or the Eastern Highlands, is a cordillera system in eastern Australia consisting of an expansive collection of mountain ranges, plateaus and rolling hills, that runs roughly parallel to the east coast of Australia and forms the fifth-longest land-based mountain chain in the world, and the longest entirely within a single country. It is mainland Australia's most substantial topographic feature and serves as the definitive watershed for the river systems in eastern Australia, hence the name. The Great Dividing Range stretches more than from Dauan Island in the Torres Strait off the northern tip of Cape York Peninsula, running the entire length of the eastern coastline through Queensland and New South Wales, then turning west across Victoria before finally fading into the Wimmera plains as rolling hills west of the Grampians region. The width of the Range varies from about to over .Shaw, John H., ''Col ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Bartle Frere
Mount Bartle Frere (pronunciation [ˈmæɔnt̥ ˈbɐːɾəɫ ˈfɹɪə]; Ngajanji: Choorechillum) is the highest mountain in Queensland at an elevation of . The mountain was named after Sir Henry Bartle Frere, 1st Baronet, Sir Henry Bartle Frere, a British colonial administrator and then president of the Royal Geographical Society by George Elphinstone Dalrymple in 1873. Bartle Frere was British Governor of Cape Colony at the outset of the Anglo-Zulu War. It is located south of Cairns, Queensland, Cairns in the Wooroonooran National Park southwest of the town of Babinda, Queensland, Babinda on the eastern edge of the Atherton Tablelands. Mount Bartle Frere is part of the Bellenden Ker Range and the watershed of Russell River (Queensland), Russell River. The foothill to summit is entirely covered by rainforest, ranging from typical tropical rainforest in the lowlands to low cloud forest at the cooler summit, where temperatures are up to 10 °C (18 °F) lower than on t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropical Rainforest
Tropical rainforests are rainforests that occur in areas of tropical rainforest climate in which there is no dry season – all months have an average precipitation of at least 60 mm – and may also be referred to as ''lowland equatorial evergreen rainforest''. True rainforests are typically found between 10 degrees north and south of the equator (see map); they are a sub-set of the tropical forest biome that occurs roughly within the 28-degree latitudes (in the equatorial zone between the Tropic of Cancer and Tropic of Capricorn). Within the World Wildlife Fund's biome classification, tropical rainforests are a type of tropical moist broadleaf forest (or tropical wet forest) that also includes the more extensive seasonal tropical forests. Overview Tropical rainforests are characterized by two words: hot and wet. Mean monthly temperatures exceed during all months of the year. Average annual rainfall is no less than and can exceed although it typically lies betwe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Johnstone River
The Johnstone River, comprising the North Johnstone River and the South Johnstone River, is a river system located in Far North Queensland, Far North and North Queensland, North Queensland, Australia. The headwaters of the river system rise in the Atherton Tablelands. The north branch of the river system rises below Merivale, flows over the Malanda Falls and through the town of and then flows generally south by east, around Francis Range and over the Jones Falls (Queensland), Jones Falls, before flowing east, covering a distance of . The south branch of the river system rises below Mount Father Clancy, southwest of Mungalli, and generally flows east over Binda Falls, through the settlement of , before flowing north, covering a distance of . The two rivers reach their confluence to form the Johnstone River east of the town of , and just west of the mouth (river), river mouth. The main river then flows east, north of the Moresby Range National Park, and empties into the Coral ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Johnstone River
The Johnstone River, comprising the North Johnstone River and the South Johnstone River, is a river system located in Far North and North Queensland, Australia. The headwaters of the river system rise in the Atherton Tablelands. The north branch of the river system rises below Merivale, flows over the Malanda Falls and through the town of and then flows generally south by east, around Francis Range and over the Jones Falls, before flowing east, covering a distance of . The south branch of the river system rises below Mount Father Clancy, southwest of Mungalli, and generally flows east over Binda Falls, through the settlement of , before flowing north, covering a distance of . The two rivers reach their confluence to form the Johnstone River east of the town of , and just west of the river mouth. The main river then flows east, north of the Moresby Range National Park, and empties into the Coral Sea. Together, the combined rivers flow over from source to mouth and desc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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