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Where do the Shrieking Sixties winds blow?
At 60° South latitude, the atmosphere encounters the "Screaming" or "Shrieking" Sixties. These winds are located in the subpolar low-pressure belt. The unique atmospheric conditions here involve extremely cold air rushing to meet warmer air from the north, creating intense low-pressure systems. TheRead more
At 60° South latitude, the atmosphere encounters the “Screaming” or “Shrieking” Sixties. These winds are located in the subpolar low-pressure belt. The unique atmospheric conditions here involve extremely cold air rushing to meet warmer air from the north, creating intense low-pressure systems. The term “shrieking” comes from the sound the wind makes as it passes through a ship’s rigging. For children learning about the globe, it is important to note that these winds are restricted to the South because the North Pole is surrounded by land, which prevents such uniform and violent wind belts from forming.
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See lessWhat does the word monsoon mean?
Monsoons are periodic winds characterized by a complete reversal of direction from one season to another. During the summer, the land heats up much faster than the ocean, creating a low-pressure zone that draws in moist air from the sea, leading to heavy rains. In the winter, the land cools faster tRead more
Monsoons are periodic winds characterized by a complete reversal of direction from one season to another. During the summer, the land heats up much faster than the ocean, creating a low-pressure zone that draws in moist air from the sea, leading to heavy rains. In the winter, the land cools faster than the sea, creating high pressure that pushes dry air back out toward the ocean. While most famous in South Asia (India), monsoon systems also exist in Africa, Australia and parts of the Americas.
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See lessWhat are the warm, dry local winds blowing in the northern part of the Alps Mountains called? (A) Khamsin (B) Sirocco (C) Chinook (D) Foehn
The Foehn wind is a European relative of the American Chinook. It is particularly well-known in countries like Switzerland, Germany and Austria. As the wind descends the northern valleys of the Alps, it brings a sudden rise in temperature and very clear visibility. For local residents, the Foehn isRead more
The Foehn wind is a European relative of the American Chinook. It is particularly well-known in countries like Switzerland, Germany and Austria. As the wind descends the northern valleys of the Alps, it brings a sudden rise in temperature and very clear visibility. For local residents, the Foehn is famous for “eating” the winter snow and triggering the start of spring. However, it is also associated with a phenomenon called “Foehn-sickness,” where the rapid change in air pressure and temperature is said to cause headaches and irritability in some people living in the mountain valleys.
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See lessWhat is the effect of Chinook winds on the central plains of the USA?
The most famous effect of a Chinook wind is its ability to change the season in a single afternoon. In the winter, the central plains are often covered in deep snow and sub-zero air. When a Chinook arrives, the temperature can jump by 20 degrees Celsius in just a few hours. This happens because theRead more
The most famous effect of a Chinook wind is its ability to change the season in a single afternoon. In the winter, the central plains are often covered in deep snow and sub-zero air. When a Chinook arrives, the temperature can jump by 20 degrees Celsius in just a few hours. This happens because the air loses its moisture on the mountains and heats up as it is squeezed while descending to lower altitudes. This warming is vital for agriculture and livestock, as it melts the snow cover, allowing animals to graze on the grass hidden beneath.
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See lessBy what name is the warm, dry and dusty local wind descending from the high mountainous regions in New Zealand known?
The Nor'wester is a significant weather event in New Zealand. As moisture-laden winds from the Tasman Sea hit the high Southern Alps, they rise and lose their water as rain on the "West Coast." When the wind crosses the peaks and descends into the Canterbury region, it is compressed and warmed by thRead more
The Nor’wester is a significant weather event in New Zealand. As moisture-laden winds from the Tasman Sea hit the high Southern Alps, they rise and lose their water as rain on the “West Coast.” When the wind crosses the peaks and descends into the Canterbury region, it is compressed and warmed by the atmosphere. This results in a hot, parched wind that can dry out soil and crops very quickly. Students can identify it by the “Nor’west arch,” a unique, long cloud formation that sits high in the sky over the mountains while the plains remain sunny.
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