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Understanding Mid-Latitude Cyclones in South Africa

May 24, 2025

Lecture Notes: Mid-Latitude Cyclones

Introduction

  • Speaker: Ana
  • Topic: Mid-Latitude Cyclones
  • Context: South African weather phenomenon occurring mainly in winter, particularly affecting South Africa.

Overview of Mid-Latitude Cyclones

  • Definition:
    • Low-pressure weather condition
    • Occurs in winter between 30° to 60° latitudes
    • Moves eastwards (from west to east)
  • Characteristics of Low Pressure:
    • Associated with rising air
    • Northern Hemisphere: Air rises anticlockwise (counterclockwise)
    • Southern Hemisphere: Air rises clockwise

Occurrence

  • Season: Winter
  • Location: Between 30° to 60° latitudes (mid-latitude region)
  • Movement: Eastwards due to westerly winds

Formation Stages of Mid-Latitude Cyclones

1. Initial Stage

  • Latitude Line: 60° latitude, called the Polar Front
  • Wind Movements:
    • Polar Easterlies: Move from east to west
    • Tropical Westerlies: Move from west to east
  • Interactions: Polar Easterlies move north, forcing Tropical Westerlies south, but do not mix.

2. Wave Formation Stage

  • Air Movements:
    • Polar Easterlies uplift warm air, causing a low-pressure area
  • Formation: Leads to a wave pattern where warm air rises sharply

3. Mature Stage (Most Important)

  • Diagram: Important to draw cross-section diagrams
  • Fronts:
    • Warm Front: Warm air sector
    • Cold Front: Cold air sector
  • Weather Map Representation:
    • Cold Front: Depicted with spikes
    • Warm Front: Smooth line
  • Weather Conditions:
    • Warm Sector: Light, warm air
    • Cold Front: Heavy, dense air causing uplift and formation of cumulus clouds
    • Heavy precipitation occurs behind the warm front, light precipitation in front
  • Movement: Cyclone moves on a circular path
    • Southern Hemisphere: Clockwise
    • Northern Hemisphere: Counterclockwise

4. Occluded Stage

  • Description: Cold front catches up with the warm front, leading to uplift
  • Outcome: Mixing of cold and warm air masses

5. Dissipating Stage

  • Final Stage: Cold front fully mixes with warm front
  • Result: Cyclone dissipates

Conclusion

  • Key Points:
    • Understand each stage for full understanding and exam success
    • Engage with content through drawing and reviewing videos
  • Next Topic: Transition to Tropical Cyclones

  • Action Items:
    • Like, subscribe, and engage with video content for further understanding.