Start studying Meteorology Chapter 7. Learn vocabulary, terms, and more with flashcards, games, and other study tools. ... Chinook winds, land-sea breezes and Santa Ana winds are examples of _____ circulations. ... Meteorology Chapter 14. THIS SET IS OFTEN IN FOLDERS WITH... 30 terms. Meteorology Chapter 9.
Chinook winds are named for the Chinook Native Americans who lived in the coastal regions of Washington and ... they are known as the Santa Ana winds. Rapid rise. Chinook winds develop when ...
The term Chinook wind is also used in British Columbia, and is the original usage, being rooted in the lore of coastal tribes and brought to Alberta by the fur-traders. Such winds are extremely wet and warm and arrive off the western coast of North America from the southwest.
They have exotic names like Chinook, Santa Ana and Taku. They “eat” snow, feed wildfires and can cause planes to crash. But what do they all have in common? They are all a type of wind.
The Santa Ana Winds. Named after Southern California's Santa Ana Canyon and a fixture of local legend and literature, the Santa Ana is a blustery, dry and warm (often hot) wind that blows out of the desert.
The Santa Ana winds are strong, extremely dry downslope winds that originate inland and affect coastal Southern California and northern Baja California.They originate from cool, dry high-pressure air masses in the Great Basin.. Santa Ana winds are known for the hot, dry weather that they bring in autumn (often the hottest of the year), but they can also arise at other times of the year.
Santa Ana wind or Chinook wind. A strong, usually cold, downslope wind is called a: katabatic wind. ... Santa Ana winds warm by _____ as they flow down an elevated desert plateau. compression. The Santa Ana wind is a _____ wind that blows into southern California. warm, dry.
What is a Chinook? By Erika Tucker. ... Witzel added some fun Chinook facts: the Santa Ana winds of California are the same thing, and in Europe, they’re called Foehn winds.
SANTA ANA ORIGINATION: The Santa Ana winds are a relative of the Chinook winds, a.k.a. the Foehn winds. However, unlike the Chinook winds which blow down the Rocky Mountains first as cold air until warmed by compression, the Santa Ana winds are often already warm and definitely dry.
Chinook, Santa Ana and Katabatic winds are those that flow downslope in response to the distribution of high- and low-pressure systems over and near large mountain areas, where compressing of descending air leads to adiabatic warming.