The su polar low lies along the polar jet stream :)
Ferrel.
Awesome kids
The convection cell that lies to the north of the polar jet stream is called the Polar Cell. This cell is characterized by cold air descending near the poles and moving toward the equator at the surface, creating a circulation pattern that influences weather patterns in polar regions. The Polar Cell operates alongside the Ferrel Cell and the Hadley Cell, contributing to the overall atmospheric circulation.
The convection cell that connects the polar jet stream and the subtropical jet stream is known as the Ferrel Cell. This cell operates between the polar cell and the Hadley cell, facilitating the movement of air and influencing weather patterns. The Ferrel Cell plays a crucial role in the dynamics of the mid-latitude atmosphere, where it helps to transfer energy and moisture between these two jet streams.
The jet stream moves faster in winter primarily due to the larger temperature differences between the polar regions and the equator. During winter, the polar air masses become much colder, while the warmer air from the south remains relatively stable. This steep temperature gradient enhances the wind speeds of the jet stream, causing it to flow more rapidly. Additionally, the winter months lead to a more pronounced and stable jet stream pattern, contributing to its increased speed.
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High or low pressure lies along the subtropical jet stream, depending on the time of year. The pressure gradient follows the path of the jet stream.
A. The subtropical jet stream lies between the westerlies and polar easterlies; this statement is true. B. The polar jet stream typically flows to the east, while the subtropical jet stream flows towards the west.
The Subpolar Low-Pressure Belt lies along the polar jet stream. It is found between 50 and 70 degrees North latitude. It consists of the Aleutian and Icelandic lows.
The polar jet stream is generally stronger than the subtropical jet stream. The subtropical jet stream lies between the westerlies and trade winds.
The subtropical jet lies just poleward of the ITCZ.
The polar jet stream is generally stronger and faster-moving than the subtropical jet stream. The polar jet stream forms at higher latitudes and is located closer to the poles, while the subtropical jet stream is located at lower latitudes. The polar jet stream is associated with larger temperature contrasts and stronger pressure gradients, resulting in stronger winds compared to the subtropical jet stream.
A continental jet-stream travels parallel to the equator - a polar jet-stream travels in a north/south direction.
The convection cell that lies to the north of the polar jet stream is the polar cell. This cell is one of the three major atmospheric circulation cells and is characterized by cold air descending at the poles, flowing towards the equator at the surface, and rising again at around 60 degrees latitude. The polar jet stream, which is a fast-flowing air current, forms at the boundary between the polar cell and the mid-latitude Ferrel cell.
The polar jet stream is generally stronger than the subtropical jet stream
The polar jet stream is generally stronger than the subtropical jet stream
Doldrums: High precipitation, little winds Horse latitudes: The trade winds and westerlies originate here Subpolar low: Lies along the polar jet stream -Apex- :)