The clockwise deflection of air in the cells near the poles is known as the Coriolis effect. This phenomenon results from the Earth's rotation, causing moving air and water to turn and twist rather than move in straight lines. In the polar regions, this deflection contributes to the formation of polar easterlies, which are prevailing winds that blow from east to west.
Polar Circulation
The clockwise deflection of air in the cells near the poles is known as the polar cell. In the polar cell, cold air descends at the poles and flows outward toward lower latitudes, where it is deflected to the right due to the Coriolis effect, resulting in a clockwise circulation in the Northern Hemisphere.
The clockwise deflection of air in the cells near the poles is known as the "polar cell." In the polar regions, cold air sinks and moves towards the equator, and due to the Coriolis effect, it is deflected to the right in the Northern Hemisphere, creating this clockwise circulation pattern.
A high-pressure system that spins clockwise is called an anticyclone. They spin clockwise in the northern hemisphere and counterclockwise in the southern hemisphere.
the equator
Polar Circulation
Polar Circulation
tne name of the semicircle joining the poles to poles is called merdian
tne name of the semicircle joining the poles to poles is called merdian
Bamboo or Kawayan in tagalog
Another name for ice at the poles is polar ice or polar ice caps.
Poles
Poles.
A high-pressure system that spins clockwise is called an anticyclone. They spin clockwise in the northern hemisphere and counterclockwise in the southern hemisphere.
A Magnet
Anaphase II is the stage of meiosis in which chromatids are separated to opposite poles of the cell. This leads to the formation of haploid daughter cells with distinct chromosomes.
Ferrel cells are the name of the cells in the middle latitudes.