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GEO • SHS 1Term 2WAEC / WASSCE SyllabusVIP Lesson

Weather, Climate and Climate Classification

Elements of weather and instruments, factors controlling climate, air masses in West Africa (cT vs. mT), the ITCZ, and the Köppen system.

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Real-World Context & Relevance in Ghana

During December to February, the Harmattan winds shroud Accra and northern Ghana in dusty haze, causing respiratory ailments and flight delays.

Key Syllabus Learning Objectives

  • 1Differentiate between weather and climate and list standard meteorological instruments
  • 2Analyze the dual roles of the Southwest Monsoons and Northeast Trades in West Africa
  • 3Explain the seasonal movement of the ITCZ and its impact on rainfall regimes in Ghana
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Comprehensive Syllabus Study Notes

• Weather vs. Climate: Weather is the day-to-day atmospheric conditions of a place; Climate is the average weather conditions over a long period (at least 30–35 years). • Elements & Instruments: Temperature (Stevenson screen, Six's thermometer), Atmospheric pressure (Barometer), Wind speed (Anemometer), Wind direction (Wind vane), Rainfall (Rain gauge), Relative humidity (Hygrometer). • West African Air Masses & Rainfall: - Tropical Maritime (mT) Air Mass: Originates over the South Atlantic Ocean; warm, moist, southwest winds bringing rainy seasons. - Tropical Continental (cT) Air Mass: Originates over the Sahara Desert; dry, dusty, northeast trade winds bringing the dry Harmattan season. - Inter-Tropical Convergence Zone (ITCZ): Low-pressure belt where mT and cT air masses meet. Its north-south migration dictates the wet and dry seasons across West Africa.
  • Weather vs. Climate: Weather is the day-to-day atmospheric conditions of a place; Climate is the average weather conditions over a long period (at least 30–35 years).
  • Elements & Instruments: Temperature (Stevenson screen, Six's thermometer), Atmospheric pressure (Barometer), Wind speed (Anemometer), Wind direction (Wind vane), Rainfall (Rain gauge), Relative humidity (Hygrometer).
  • West African Air Masses & Rainfall:
  • Tropical Maritime (mT) Air Mass: Originates over the South Atlantic Ocean; warm, moist, southwest winds bringing rainy seasons.
  • Tropical Continental (cT) Air Mass: Originates over the Sahara Desert; dry, dusty, northeast trade winds bringing the dry Harmattan season.
  • Inter-Tropical Convergence Zone (ITCZ): Low-pressure belt where mT and cT air masses meet. Its north-south migration dictates the wet and dry seasons across West Africa.
Practical Example:

During December to February, the Harmattan winds shroud Accra and northern Ghana in dusty haze, causing respiratory ailments and flight delays.

Core Takeaway:

In WASSCE climate graphs, rainfall is plotted as vertical bars (histograms) while temperature is plotted as a smooth continuous line.

WAEC / WASSCE Examiner Tips
  • In WASSCE climate graphs, rainfall is plotted as vertical bars (histograms) while temperature is plotted as a smooth continuous line.
Common Candidate Pitfalls & Errors to Avoid
  • Answering a weather question with climate material, or vice versa, instead of separating the short state of the atmosphere from the long average.
  • Adding twelve monthly means and reporting the total as the annual mean temperature.
  • Reporting the annual temperature range as the highest monthly temperature.
  • Saying temperature rises with height, so the lapse rate is applied in the wrong direction on a hill station.
  • Treating relative humidity as the amount of water in the air, when it is a percentage of what that temperature could hold.
  • Applying the lapse rate to the height above sea level instead of the height difference between the two stations.
Topic Mastery Checklist
  • Differentiate between weather and climate and list standard meteorological instruments
  • Analyze the dual roles of the Southwest Monsoons and Northeast Trades in West Africa
  • Explain the seasonal movement of the ITCZ and its impact on rainfall regimes in Ghana
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