The tempurate differences creates the jet stream. Wind is caused by the uneven heating of earth's surface and the differences of air pressure. Cold polar air creates low air pressure and a cold surface which creates wind.
The jet stream
Minnesota receives arctic air when the polar jet stream moves south across Canada.
Polar 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.
The northernmost (and/or southernmost) of the various jet streams that circle the Earth.
The polar jet stream significantly influences temperature by acting as a boundary between cold polar air and warmer air from the tropics. When the jet stream dips southward, it can bring colder Arctic air to lower latitudes, resulting in cooler temperatures in those regions. Conversely, when it shifts northward, it allows warmer air to move into areas that would typically be cooler, leading to higher temperatures. This dynamic movement of the jet stream can create extreme weather patterns and temperature fluctuations.
The polar easterlies are cold winds that flow from the polar regions toward the equator, while the jet stream is a fast-flowing river of air high in the atmosphere that influences weather patterns. Together, they can interact to create significant weather changes in the U.S., particularly in winter. When the polar easterlies are strong, they can push the jet stream southward, bringing cold Arctic air into the continental U.S., which can lead to frigid temperatures and winter storms. Conversely, if the jet stream is positioned further north, it can allow for warmer air to move in, moderating temperatures in many regions.
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.
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 polar jet stream is generally stronger than the subtropical jet stream