http://en.wikipedia.org/wiki/Polar_high
The 7 components of the general circulation pattern in the atmosphere are: the Intertropical Convergence Zone (ITCZ), the subtropical highs, the subpolar lows, the polar highs, the polar easterlies, the westerly winds, and the jet streams.
False. Easterly waves are typically associated with tropical waves that move from east to west across tropical regions. They are often a precursor to the formation of tropical cyclones and are linked to the Intertropical Convergence Zone rather than polar highs.
Polar easterlies are dry, cold prevailing winds that blow from the east. They emanate from the polar highs, areas of high pressure around the North and South Poles. Polar easterlies flow to low-pressure areas in sub-polar regions. Westerlies are prevailing winds that blow from the west at midlatitudes.
The main global wind systems are the Trade Winds, Westerlies, and Polar Easterlies. Trade Winds blow from the subtropical high pressure belts towards the equator, Westerlies blow from the mid-latitudes towards the poles, and Polar Easterlies blow from the polar highs towards the mid-latitudes. These wind systems are influenced by the Earth's rotation (Coriolis effect) and the temperature differences between different regions.
This usually refers to temperatures.
The 7 components of the general circulation pattern in the atmosphere are: the Intertropical Convergence Zone (ITCZ), the subtropical highs, the subpolar lows, the polar highs, the polar easterlies, the westerly winds, and the jet streams.
The dry, cold winds originating from the Polar Highs, from high pressure zones.
False. Easterly waves are typically associated with tropical waves that move from east to west across tropical regions. They are often a precursor to the formation of tropical cyclones and are linked to the Intertropical Convergence Zone rather than polar highs.
Polar easterlies are found in the polar regions of Earth, specifically within the Arctic and Antarctic Circles. These winds blow from the east and are typically characterized by cold air descending from the polar highs. They occur between 60 degrees latitude and the poles, influencing weather patterns in these extreme latitudes.
Polar easterlies are associated with cold, dry air that originates from the polar regions. These winds blow from the east towards the west and are produced as cold air sinks and spreads out from the polar highs. The air is typically stable and can lead to clear skies, but it can also contribute to frigid temperatures in the regions they influence.
Bipolar is an condition where a person experiences extreme highs and lows in there moods. It is psychologically similar to schizophrenia. But they are treatable with anti-psychotics and mood stabilizers.
The polar easterlies (also Polar Hadley cells) are the dry, cold prevailing winds that blow from the high-pressure areas of the polar highs at the north and south poles towards low-pressure areas within the Westerlies at high latitudes.
Highs: Everything. Lows: Nothing.
acrophobia is a phobia of extreme highs
Greatest Highs was created in 1998.
Thomas Highs died in 1803.
Polar easterlies are dry, cold prevailing winds that blow from the east. They emanate from the polar highs, areas of high pressure around the North and South Poles. Polar easterlies flow to low-pressure areas in sub-polar regions. Westerlies are prevailing winds that blow from the west at midlatitudes.