S t a t i o n |
D a t e |
T i m e |
T em p erat u r e, A i r a t 1 . 5 m | T em p erat u r e, Soi l a t 1 0 c m |
d e gr ee s C elsius | d e gr ee s C elsius | |||
Swaziland | 15/8/18 | 1 2 : 0 0 am | 16.0 |
28.5 |
15/8/18 | 2 : 0 0 am | 18.8 |
30.2 |
|
15/8/18 | 4 : 0 0 am | 17.5 |
33.8 |
|
15/8/18 | 6 : 0 0 am | 20.9 | 38.7 | |
15/8/18 | 8 : 0 0 am |
23.3 |
42.1 |
|
15/8/18 | 1 0 : 0 0 am |
25.8 |
46.8 |
|
15/8/18 | 1 2 : 0 0 pm |
33.0 |
50.6 |
|
15/8/18 | 2 : 0 0 pm |
40.6 |
54.5 |
|
15/8/18 | 4 : 0 0 pm |
39.9 |
52.7 |
|
15/8/18 | 6 : 0 0 pm |
37.8 |
49.5 |
|
15/8/18 | 8 : 0 0 pm |
32.0 |
45.8 | |
15/8/18 | 1 0 : 0 0 pm |
28.7 |
38.4 |
|
15/8/18 | 1 2 : 0 0 am |
22.2 |
30.6 |
Graph of Temperature
Finding the range of the temperatures:
Soil Temperatures ( d e gr ee s C elsius )
Highest temperature: 54.5
Lowest temperature: 28.5
Range of the temperature: 26.0
Air temperature ( d e gr ee s C elsius )
Highest temperature: 40.65
Lowest temperature: 16.0
Range of the temperature: 24.65
Data Analysis
As the air temperature increases, the temperature of the soil also increases. When the air temperature reduces, so does the soil temperature reduces.
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In case cold weather would pass the area, the air temperature would drastically drop whereas the soil temperature would slightly drop.
Based on the graphs, the soil temperature is usually much higher than the temperature of the air at any given time. For this reason, the air is the main determinant of the temperature of the soil. Even though the air temperature may reduce at any time, the rate of temperature reduction for the soil temperature is much lower. As such the soil temperature can be said to be more stable irrespective of other conditions.
Conclusion
For the people involved in farming and agriculture, the data shows the need to determine the kinds of plants that can sustain higher temperature. This is to ensure survival rate for the crops. The data also shows the need for farmers to consider planting seasons and the types of irrigation for better productivity.