At what latitude does the Jet Stream typically flow?

The Jet Stream typically flows at higher latitudes, particularly around 30 to 60 degrees North and South. It is primarily located in the mid-latitudes, where it serves as a boundary between the warmer air of the tropics and the colder air from the poles. This is because the Jet Stream is influenced by the temperature differential between these two regions, leading to the formation of strong winds at those latitudes.

While there are multiple jet streams that can exist at various latitudes, the most significant and well-known ones are found between 30 and 60 degrees, especially where extratropical cyclones and anticyclones develop. At the equator, the lack of temperature differences and the Coriolis effect are not conducive to strong wind patterns like the Jet Stream. Similarly, at 90 degrees North and South, the polar regions have calmer winds due to their unique climatic conditions, which do not create the same dynamic atmospheric interactions found in the mid-latitudes.

Thus, the flow of the Jet Stream is most accurately described by its typical presence around 60 degrees North and South, aligning with the characteristics that influence its formation and the atmospheric dynamics at those latitudes.