no
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.
When warmer air lies above polar air, it creates an unstable atmosphere. The temperature difference can lead to the formation of unstable weather conditions such as thunderstorms, strong winds, and storm systems. This can result in more extreme weather patterns and changes in atmospheric pressure.
Intertropical convergence zone: lies roughly along the equator.Horse latitudes: lies along the subtropical jet stream.Subpolar low: connects the polar cell and the Ferrel cell.
The Salton Sea
A channel of an ephemeral stream always lies above the water table and only has water flowing through it as the direct response to recent and local precipitation.
Doldrums: High precipitation, little winds Horse latitudes: The trade winds and westerlies originate here Subpolar low: Lies along the polar jet stream -Apex- :)
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 a high-altitude air current found in the upper atmosphere near the Earth's poles. It meanders and shifts in response to differences in temperature and pressure, influencing weather patterns. It plays a key role in steering storm systems and determining the track of weather systems in mid-latitudes.
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 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 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 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 Polar cell lies to the north of the Polar jet stream in the atmosphere. This cell is characterized by cool air sinking at the poles, moving towards lower latitudes at the surface, and then rising at around 60° latitude to complete the circulation loop.
When warmer air lies above polar air, it creates an unstable atmosphere. The temperature difference can lead to the formation of unstable weather conditions such as thunderstorms, strong winds, and storm systems. This can result in more extreme weather patterns and changes in atmospheric pressure.
No, the doldrums, also known as the Intertropical Convergence Zone (ITCZ), lies between approximately 5 degrees north and 5 degrees south of the equator. This region is characterized by calm winds and often leads to significant rainfall. The area between 30 and 40 degrees north is typically associated with the prevailing westerlies and is not part of the doldrums.