Weather Data (Cambridge International IGCSE Geography)
Calculations using Weather Data
Spec point —
2.4.2· Make calculations using information from weather instruments
Rainfall
- Daily, weekly, monthly and annual rainfall totals
- Always measured in mm
- Always plotted on a bar graph
- Mean (average) monthly and annual rainfall over a minimum of 30 years
Annual Rainfall Amounts
| Annual rainfall in mm | Description of the amount |
|---|---|
| 0 - 249 | Very low |
| 250 - 499 | Low |
| 500 - 999 | Moderate |
| 1000 - 1999 | High |
| Over 2000 | Very high |
Temperature
-
Measured in °C or °F
-
Always plotted as a line graph
-
Calculations are:
- Diurnal (daily)
- Mean daily temperature
- Mean monthly temperature
- Annual range
- Mean annual range
Describing Temperatures
| Temperature (°C) | Description |
|---|---|
| Below -10 | Very cold |
| -10 to -1 | Cold |
| 0 - 9 | Cool |
| 10 - 19 | Warm |
| 20 29 | Hot |
| 30 and above | Very hot |
Describing Temperature Ranges
| Temperature Range in °C | Description |
|---|---|
| 0 - 3 | Very small |
| 4 - 8 | Small |
| 9 - 19 | Moderate |
| 20 and above | Large |
Wind
-
Wind is measured in speed
- Knots (Kts)
- Miles per hour (mph)
- Kilometres per hour (km/h)
-
Direction is quoted from where the wind is blowing and not where it is going to, using compass points
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This is important as it informs of what temperature and moisture are being brought with it
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The most frequently occurring wind is called the prevailing wind (UK's prevailing wind is from the southwest)
-
The direction giving the strongest wind is called the dominant wind
-
Wind is plotted on a map with wind barbs
Describing Wind Speeds
| Wind Speeds (km/h) | Description |
|---|---|
| Below 50 | Calm, light, moderate or strong winds |
| 50 - 100 | Gale |
| 101 - 118 | Storm |
| 119 and above | Hurricane |
Exam Hint
Always make sure you state wind direction clearly, for example:
- The wind is coming from the east
- It is a westerly wind
Saying the wind is in a northerly direction isn't clear enough and can be misinterpreted
Pressure
-
Pressure is measured in millibars (mb) and based against average sea level pressure
-
The mean (average) sea level pressure is 1013 mb
-
It is not totalled over time but on a time basis depending on circumstances:
- Following a storm or potential storm, pressure readings would be needed hourly or more
- Forecast for a weekend would be a daily measurement
- Forecast for sailing may need an early morning reading and then later, etc.
-
On a weather chart, lines joining places with equal sea-level pressures are called isobars
-
Isobars identify features such as anticyclones (areas of high pressure) and depressions (areas of low pressure)
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Anticyclone (high-pressure) winds tend to be light and blow in a clockwise direction (in the northern hemisphere)
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Also, the air is descending, which reduces the formation of clouds and leads to light winds and settled weather conditions
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In depressions (low pressure), the air rises and blows in an anticlockwise direction around the low (in the northern hemisphere)
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The rising air cools, causing water vapour to condense, which forms clouds and perhaps precipitation
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This is why the weather in a depression is often unsettled; there are usually weather fronts associated with depressions.
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A high-pressure area surrounded by lower pressures is described as a high-pressure system even if 1013 mb are not reached
-
Low-pressure areas surrounded by higher pressure can have a central pressure of more than 1013 mb
Describing Pressure Systems
| Pressure System in mb | Description |
|---|---|
| 1013 | Sea level pressure |
| 1013 and above | High pressure or anticyclone |
| 1013 and below | Low pressure or depression |
Relative humidity
-
This is measured using the relative humidity table. Find it by looking for the intersection of the wet bulb thermometer line's depression and the dry bulb temperature line
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Humidity is shown as a percentage of temperature
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Temperature determines relative humidity; the more water vapour the air can hold, the higher the temperature.
- If air is 20 °C and holds 4 grams of water, it has a relative humidity of 27%
- 4g more water is added, so air is now 8g @ 20°C = 52% and so on until it reaches saturation and moisture will start to condense (20°C still, but air holds 15g of water = 100% humidity)
- However, if the temperature rises, then the air can again hold more water, so the relative humidity drops (15g @ 23°C = 83% humidity or 15g @ 32°C = 50% humidity, etc.)
- But if the temperature drops, then the air holds too much water, so the excess water is released until equilibrium is reached
Worked Example Explain how a wind vane is used to show the direction from which the wind is blowing
[2 Marks]
- The arrow / pointer turns / spins round / pushed by wind [1] and points to N/E/S/W / compass direction (from which wind is blowing) [1]
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