SUBJECT: GEOGRAPHY
CLASS: SS1
DATE:
TERM: 2ND TERM
REFERENCE MATERIAL
WEEK SIX AND SEVEN
TOPIC: WEATHER AND CLIMATE
FOR WEEKS SIX AND SEVEN
Weather is defined as the condition of the atmosphere of a place at a certain time or within a short period. The weather of a place is always very brief and changes regularly e.g. the weather of a day could be sunny, rainy or cloudy etc.
Climate is defined as the average atmospheric condition of an area over a long period of time. Unlike weather, climate of a place lasts for a very long time before it can change.
Elements of Weather and Climate
The elements of weather and climate include:
(i) Temperature (ii) Rainfall
(iii) Wind (iv) Pressure
(v) Relative humidity (vi) Cloud cover
(vii) Sunshine
Climate varies from one part of the world to another due to the effects of the following factors:
Evaluation Questions:
Importance of weather and climate to man
1 Human settlement: Weather and climate affect the rate at which human being live in a place.
8 Soil Formation: Soil is formed from parent rocks which have been broken by elements of weather and climate. The rate of disintegration of rocks to form soil is principally a factor of climate.
11 Cultural Activities: The climate of a place can also affect the cultural activities of some people e.g. winter or summer sports.
Evaluation Questions:
KEEPING WEATHER RECORDS AND INSTRUMENTS
Measurement of Rainfall
An instrument called Rain-gauge is used in measuring rainfall.
Description: A rain gauge consists of a metal funnel that leads to a glass bottle enclosed within a copper cylinder .The gauge is usually erected high above the ground to avoid splashing and it is sited far away from buildings and tall trees that might shelter it. The rain gauge must be examined every day and daily records taken. Record is taken by removing the funnel and the contents of the glass bottle are emptied into the measuring cylinder.
Formula
Add total rainfall for the month
No of days in the month
(2) Annual rainfall = Add the total rainfall (Jan-Dec)
(3) Annual range of rainfall
= Month with - month with
highest rainfall lowest rainfall
(4) Mean annual rainfall =
Total rainfall (Jan- Dec)
12
(5) Highest rainfall = Month with the highest rainfall
(6) Lowest rainfall = Month with the lowest rainfall
Example: Calculate (i) month with the lowest rainfall (ii) month with the highest rainfall
(iii) annual rainfall (iv) annual range of rainfall (v) mean annual rainfall using the table below:
Month | J | F | M | A | M | J | J | A | S | O | N | D |
Rainfall | 10 | 80 | 20 | 18 | 5 | 50 | 45 | 40 | 90 | 20 | 50 | 40 |
Solutions
(i) Month with the lowest rainfall = May (5cm)
(ii) Month with the highest rainfall = September (90 cm)
(iii) Annual rainfall = Total rainfall for 12 months.
= 10 + 80 + 20 + 18 …+ 50 + 40 = 468 cm
(iv) Annual range of rainfall = 90 - 5 = 85 cm
(v) Mean annual rainfall =
Total rainfall for 12 months
12
= 468 = 39 cm
12
Measurement of Temperature
An instrument called Thermometer measures the temperature of a place.
Description: The thermometer is a narrow glass tube filled with mercury or alcohol. It works on the principle that mercury and alcohol expand when heated and contract when cooled. Temperature is commonly recorded in centigrade (oC) or Fahrenheit (oF) scale. The freezing (lowest) point for centigrade scale is 0oc while Fahrenheit is 320F. The boiling (or highest) point for centigrade scale is 100oC while that of the Fahrenheit is 212oF. It is possible to convert from one scale to another.
Geographers are interested in shade temperatures which is the temperature of the air to exclude the intensity of the suns radiant heat. To get accurate records, thermometers are kept in a standard shelter called Stevenson Screen to protect it from the effects of radiant heat of the sun and rain. The Stevenson screen is a wooden box raised above the ground to a height of 4ft or 1.2m.To measure the maximum and minimum temperatures of the day, a combined maximum and minimum thermometers are used.
Calculations:
Formulae
(i) Mean daily temperature = Max. temp. + Mini temp. for a day
2
(ii) Diurnal range of temperature = Max. temp – Mini. Temp that day
(iii) Monthly range of temperature = Difference between the hottest and the coldest daily temperature for the month.
(iv) Annual temperature = temperature of the hottest month - temperature of the coldest month.
(v) Annual temperature = Total temperature (Jan – Dec)
(vi) Mean Annual Temperature = total temp (Jan – Dec)
12
Example: Calculate using the table below
(i) The month with the highest temperature
(ii) The month with the lowest temperature
(iii) Annual range of temperature
(iv) Annual temperature
(v) Mean annual temperature
Month | J | F | M | A | M | J | J | A | S | O | N | D |
Tem.(0o) | 40 | 30 | 21 | 25 | 10 | 40 | 48 | 30 | 25 | 30 | 20 | 15 |
(i) Month with the highest temperature = July (48oc)
(ii) Month with the lowest temperature = May (10oc)
(iii) Annual range of temperature = temp of the hottest month – Temp of coldest
= 48oc – 10oc
= 38oc
(iv) Annual temperature = Total temp.(Jan – Dec) = 40 + 30 + 21
+…… + 30 + 20 + 15
= 334oc
(v) Mean annual temperature = Total temp (Jan – Dec)
12
= 334
12
= 27.8oc
Measurement of Wind
Wind has direction and speed. The direction of wind is measured by an instrument called Wind Vane while the speed of the wind is measured by a different instrument called Anemometer.
Description: (a) Wind vane: wind vane is made up of two parts – one part is the arrow or vane on the top, which is free to move with the prevailing wind. The other part is stationary and consists of a frame and four compass points. The vane or arrow points to the direction from which the wind is blowing so that wind is named from the direction it blows eg South West Wind blows from South West direction. Wind vane is located in an exposed position so that tall buildings and trees do not deflect the wind direction.
(b) Anemometer: This consists of three or four semi-circular cups attached to the ends of horizontal spokes mounted on a high vertical spindle. As the wind blows, the cups rotate. The higher the speed of the wind, the greater the speed of the cups and vice versa.
Measurement of pressure
The instrument used in measuring atmospheric pressure is called Barometer. Pressure is measured in unit of force called milibars A normal atmospheric pressure shows a reading of 760mm (76cm) or 1013 millibars. Mercury barometer consists of a beaker in which a glass tube is dipped and both contain mercury. Another instrument used for measuring pressure is the aneroid barometer. But a modified aneroid barometer used in aeroplanes is called Altimeter.
Measurement of Relative Humidity
The instrument used for measuring relative humidity is called Hygrometer.
Description: The hygrometer consists of wet and dry-bulb thermometers placed side by side in the stevension screen. The dry bulb is an ordinary thermometer that measures the shade temperature. The wet-bulb is kept by a wick that is dipped in a container of distilled water. When the air is not saturated, evaporation, which produces a cooling effect, takes place from the moist wick. The wet bulb always shows a lower reading than the dry bulb. The difference in the two readings, if high, indicates low humidity and if low, indicates high humidity. If there is no difference in their readings, it means that the air is saturated and therefore, the relative humidity would be 100 %.
Evaluation Questions:
How do we calculate:
General Evaluation Questions:
Reading Assignment
Read on weather and climate in Essential Geography Pgs. 75-77
Weekend Assignment
(b) Humidity (c) Latitude (d) Natural Vegetation
(b) Thermometer (c) Anemometer (d) Rain guage
(b) Relative humidity (c) Temperature (d) Wind speed
Theory
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