The given graphs demonstrate the regional amount of rain and temperature degree in one of the East African sites. The rainfall is measured in milimetres and temperature scaled in degrees.
Overall, it can be clearly seen that the local temperature is thoroughly proportional to the rain scope which falls each month in the given area. Also, spring and autumn months are featured by most frequent rainfalls and warmth respectively.
According to the bar graph, winters in this region are almostly rainless (below 25 milimetres) except December. Similarly, in summer there are fewer rainfall degrees comparing to spring and autumn as well. The obvious fluctuation is shown in an annual rain falling tendency which sharply increases in March and hits a peak at approximately 300 mm in April. Then it rapidly drops to 150 milimetres in May and totally falls down to the initial height in summer. Finally, in October and Novermber it remains stable at 150 mm and declines three times in December.
The temperature changes is shown on the line graph in a form of oscillation within the year. In January it starts with 22.5 degrees and dramatically increases until March where it peaks at nearly 24. Thereafter, it gradually falls down and hits the lowest point in July at 20.5 degrees. Afterwards, the regional temperature rockets again till 23.5 in October which is followed by a sharp drop in December at about 21 degrees.