Coriolis Effect: The rotation of the Earthcauses moving air to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere, resulting in curved wind paths.
There are three primary wind patterns that influence the Earth'sclimate:
Trade Winds: These are steady easterly winds that flow towards the equator and are found between 30 degrees north and south of the equator. They are crucial for sailing and historically facilitated trade between continents.
Prevailing Westerlies: These are prevailing winds that blow from the west to the east in the mid-latitudes, between 30 and 60 degrees latitude in both hemispheres. They play a significant role in shaping weather patterns and are important for transoceanic travel.
Polar Easterlies: These are dry, cold prevailing winds that blow from the east to the west near the poles. They are formed as a result of the temperature difference between the polar regions and the equator.
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.
Earth Science
History of Earth
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.
Earth Science
History of Earth
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.
Earth Science
History of Earth
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.