Jet streams are caused by a combination of Earth's rotation on its axis and atmospheric heating by solar radiation. The Coriolis effect describes how a planet's surface and atmosphere rotate fastest relative to each other at the planet's equator while virtually not rotating at all at the poles. While this speed difference generally has very little effect on Earth's surface, it plays an important role in atmospheric air currents because air at higher levels of the atmosphere, especially near the equator, must travel very fast to keep up with the planet's rotation. Thus there is a tendency for air at higher levels of the atmosphere to "slip" and fall behind the speed of the air below. This results in a pressure buildup behind the "slipped" air, and so some air will have to catch up by moving in the same general direction as the planet's rotation (west to east on Earth); however, this air does not follow a simple pattern but instead is also influenced by its temperature and water content compared to that of surrounding air regions. In essence, instead of the atmosphere moving along with the planet consistently, parts of the atmosphere travel faster than others via jet streams.
Jet streams form near boundaries of adjacent air masses with significant differences in temperature, such as the polar region and the warmer air towards the equator.
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. 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 jet stream is typically faster in the winter due to greater temperature contrasts between polar and tropical regions. This temperature difference creates stronger winds that drive the jet stream at higher speeds during the winter months.
The weatherman said that the latest jet stream would bring more cold air to the region on Friday. The jet flew over Wichita, leaving a trail of jet stream behind it.
The jet stream is a fast-flowing, narrow air current in the upper atmosphere that influences the movement of weather systems. Changes in the jet stream's position and strength can impact the direction and speed of surface winds. The jet stream's meandering path can cause shifts in the pressure systems on the ground, which in turn affect wind patterns at the surface.
The jet stream
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.
mid latitude jet stream and jet stream
jet stream
No. The jet stream is in the upper troposphere and lower stratosphere.
The polar jet stream is generally stronger than the subtropical jet stream
The polar jet stream is generally stronger than the subtropical jet stream
A jet stream can increase ground speed by up to 200 mph if going the same direction. But it may be a bumpy ride.
a jet stream is important because of climate control
a jet stream is important because of climate control
It is false that a plane flying against a jet stream will travel faster than a plane traveling with a jet stream.