Polar jet stream is stronger.
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.
Jet streams are fast, narrow air currents in the atmosphere, typically found at high altitudes between 7 and 12 kilometers. They flow from west to east due to the Earth's rotation. Jet streams play a significant role in shaping weather patterns and can influence the movement of storms.
The temperature difference between the polar region and the mid-latitudes is greater in winter, leading to a stronger temperature gradient. This increased temperature gradient results in a stronger polar front jet stream during the winter months.
Wind doesn't control the jet stream; this is controlled by something much more complex. It has to do with the mass balance of the atmosphere, vertically propagating waves, and the earth's rotation.
The northernmost (and/or southernmost) of the various jet streams that circle the Earth.
The polar jet stream is generally stronger than the subtropical jet stream
The polar jet stream is generally stronger than the subtropical jet stream
The polar jet stream is generally stronger than the subtropical jet stream
The polar jet stream is generally stronger than the subtropical jet stream. The subtropical jet stream lies between the westerlies and trade winds.
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.
ferrel
Ferrel.
The two jet streams in the Southern Hemisphere are the Subtropical Jet Stream and the Polar Jet Stream. The Subtropical Jet Stream is located closer to the equator and the Polar Jet Stream is found closer to the South Pole. These high-altitude, fast-flowing air currents play a significant role in influencing weather patterns in the Southern Hemisphere.
Ferrel
polar; subtropical
Jet streams are fast, narrow air currents in the atmosphere, typically found at high altitudes between 7 and 12 kilometers. They flow from west to east due to the Earth's rotation. Jet streams play a significant role in shaping weather patterns and can influence the movement of storms.
The temperature difference between the polar region and the mid-latitudes is greater in winter, leading to a stronger temperature gradient. This increased temperature gradient results in a stronger polar front jet stream during the winter months.