SUMMARY
The polar jet stream flows counter-clockwise around the Earth due to the dynamics of the Ferrel and Polar Cells, specifically influenced by the Coriolis effect. The air at the north end of the Ferrel Cell and the south end of the Polar Cell rises, causing a circulation that is primarily eastward. Diagrams indicate that the polar jet resides in the upper northern part of the Ferrel Cell, where the circulation begins to turn southward after rising. Understanding the interaction between these cells and the Coriolis Force is crucial for comprehending the jet stream's behavior.
PREREQUISITES
- Understanding of atmospheric circulation patterns, specifically the Ferrel and Polar Cells.
- Knowledge of the Coriolis effect and its impact on wind direction.
- Familiarity with jet streams and their role in weather systems.
- Basic meteorological terminology and concepts.
NEXT STEPS
- Research the dynamics of the Ferrel and Polar Cells in greater detail.
- Study the Coriolis effect and its implications for wind patterns.
- Examine the characteristics and behavior of jet streams in different seasons.
- Explore advanced meteorological models that simulate atmospheric circulation.
USEFUL FOR
Meteorologists, atmospheric scientists, students of environmental science, and anyone interested in understanding weather patterns and jet stream dynamics.