Activities result in increased cloud cover, greenhouse gases, and aerosols in the atmosphere. However, fossil fuels are the largest contributors of carbon monoxide II gas. In turn, aerosols and greenhouse gases alter incoming solar radiation and outgoing thermal radiation at the Earth's surface (Hughes 66). In this case, this leads to cooling or warming of the climate. Historically, climate change is the result of the rise of industrialization. Most industrial activities caused air pollution. The concentration has increased over time with the intensification of industrial activities. Furthermore, increased transportation, cement production, heating and cooling of buildings are human activities that contribute to the increase of climate change. The activities mentioned use fossil fuels, which ultimately release greenhouse gases into the atmosphere. Another contributor is deforestation. On several occasions, trees or plantations absorb carbon monoxide II and decrease the absorption of the gas. At the same time, the decomposition of cut plantations releases carbon monoxide II. On the other hand, deforestation reduces the amount of carbon monoxide II absorption due to the removal of trees. Methane gas in the atmosphere has also increased equally. It is mainly produced through human activities related to landfills, agriculture, and natural gas distribution (Hansen and Makiko 23). Unlike other greenhouse gases, methane is