SUMMARY
An occluded front is formed when a cold front overtakes a warm front, as observed in the Atlantic cyclone moving North/East at coordinates 15W 58N. The merging of these fronts indicates a trough associated with low pressure and a ridge from the same system. This phenomenon is common in deep low-pressure regions and signifies ongoing weather changes, particularly in the blue and red areas of the synoptic chart. The extended nature of the occluded front suggests that the interaction between the cold and warm fronts will continue to evolve towards the southeast.
PREREQUISITES
- Understanding of synoptic charts and their components
- Knowledge of meteorological terms such as occluded front, cold front, and warm front
- Familiarity with low-pressure systems and their characteristics
- Basic grasp of weather patterns and cyclones
NEXT STEPS
- Study the dynamics of occluded fronts in meteorology
- Learn about the formation and characteristics of cyclones
- Research the impact of cold and warm fronts on weather patterns
- Examine case studies of synoptic charts illustrating occluded fronts
USEFUL FOR
Meteorology students, weather enthusiasts, and professionals analyzing weather patterns and forecasting using synoptic charts.