ferrel
The polar jet stream is generally stronger than the subtropical jet stream
The jet stream refers to a high-speed, narrow air current in the atmosphere. Jamaica does not have a jet stream of its own, as jet streams typically flow at higher altitudes in the Northern Hemisphere, affecting weather patterns globally.
polar; subtropical
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 subtropical jet stream can influence Florida's weather by steering storm systems and altering temperature patterns. When the jet stream dips southward, it can enhance the development of low-pressure systems, leading to increased rain and thunderstorms in the region. Additionally, it can help bring cooler air masses into Florida during winter months, affecting overall seasonal weather conditions.
Ferrel
Ferrel.
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.
ferrel
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 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.
The polar jet stream is generally stronger than the subtropical jet stream. The subtropical jet stream lies between the westerlies and trade winds.
The high pressure band of air blowing from west to east is known as the subtropical jet stream. It is located at high altitudes in the atmosphere and affects weather patterns in the mid-latitudes. The subtropical jet stream is stronger in the winter and weaker in the summer.
The polar jet stream is generally stronger than the subtropical jet stream
The subtropical jet lies just poleward of the ITCZ.
The jet stream is a narrow band of strong winds in the upper atmosphere that is driven by the temperature difference between air masses. Convection is the transfer of heat through the movement of fluid (in this case, air). The jet stream is influenced by the temperature contrasts created by convection, particularly between the polar and tropical air masses.
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.