Climate change is evidenced through changes in weather patterns such as winds, humidity, and temperatures for certain periods. Natural climate changes occur less frequently and are triggered by factors related to geographical aspects and solar radiation. The movement of the earth on orbit triggers climate changes that cause some areas to have higher temperatures than usual while others are significantly cold depending on the position of the earth on the orbit. The sun's heat causes changes in stratospheric ozone and increases the amount of greenhouse gases. Heat from oceanic crust also contributes to warming as a result of episodic hydrothermal vents (Liao & Sandeberg, 2012). Volcanic activity also causes the release of certain elements that can block sunlight and also contribute to increased greenhouse gases in the atmosphere. The most destructive human contribution to climate change is the burning of fossil fuels, which releases carbon dioxide and other greenhouse gases. in the atmosphere. Increased levels of carbon dioxide, methane, nitrous oxide, and halocarbons in the atmosphere cause an imbalance in the earth's energy. This is because the gases alter the solar radiation and thermal radiation that regulate Earth's energy. Research indicates that anthropogenic climate change is the cause of the increase in global warming over the past fifty years. 57% of the carbon dioxide emitted is absorbed into the atmosphere while the rest is absorbed into the oceans. Carbon dioxide in the atmosphere is the most important greenhouse gas associated with global warming (Eby, Zickfield, Montenegro, Archer, Meissner, and Weaver,