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Factors contributing to climate change coolling as well as heating our…

- - - - Methane also plays a role of greenhouse gas because it warms up the heat in Earth’s atmosphere. If emitted to the atmosphere either naturally as a result of wetland decomposition, or from anthropogenic activities such livestock digestion and fossil fuel processing methane is quite effective at absorbing heat. It does so through interaction with infrared radiation, that is component of the energies Earth receives from sunlight. Thus trapped by methane molecules, this radiation is unable to leave the planet’s surface and contributes in its heating. However short lived, methane (unlike carbon dioxide) is a marquee greenhouse gas and thus contributes to both global warming and climate change.
    - - As a greenhouse gas, nitrous oxide (N2O) warms the Earth’s atmosphere. It is also important to note that when nitrous oxide enters the atmosphere naturally or through human activities such as agricultural practices and industrial processes, it absorbs infrared radiation and hinders its escapism into space. The heat that is trapped in the earth helps to cause greenhouse effect, which heats up planet. Nitrous oxide is characterized by a long atmospheric lifetime, as it lingers in the air for several decades. It also has a high global warming potential, which translates to stronger heat-trapping ability in comparison with other greenhouse gases like carbon dioxide. Naturally, increased nitrous oxide concentrations in the atmosphere further facilitate global climate change through expanding upon its general greenhouse effect and affecting worldwide temperature patterns.
    - - CO2 serves as a heat-trapping gas due to its primary role in the planet’s natural greenhouse effect. The portion of sunlight that reaches the Earth is reflected back into space, and what does not get refracted warms up our planet. When the earth gets warmer, it gives off infrared radiation. The greenhouse gases like CO2 prevent some of this outgoing radiation from escaping and sending it into space. Rather, the retained heat is reflected back to the Earth’s surface creating a general warming known as greenhouse effect. In other words, CO2 acts like a blanket covering the Earth that provides sunlight access but does not allow some of it as heat to escape into space and maintain temperature stabilization within the atmosphere. The increased levels of CO2 concentration in the atmosphere can be attributed to human activities, particularly burning fossil fuels; this has intensified the greenhouse effect and caused global warming.
    - - Water vapor is a natural greenhouse that has an essential role to play in the modulating of Earth’s temperature. The heat from the sun warms up the earth surface and this makes water evaporate and turn into vapor which rises to form clouds. This water vapor behaves like a greenhouse gas since it retains some of the heat that is radiated by Earth to prevent them from escaping out into space. In essence, it helps to build up the greenhouse effect that is necessary for keeping a comfortable level temperature on Earth. But unlike anthropogenic greenhouse gases like carbon dioxide, water vapor levels in the troposphere are largely controlled by natural processes and not affected directly through human activities.
- - - - Axial Tilt (Obliquity):
        The axial tilt, or obliquity, varies on a 41,000-year cycle. A higher tilt results in more extreme seasons, affecting climate. This cycle contributes to the long-term modulation of Earth's climate as it influences the distribution of sunlight across latitudes over extended periods.
      - Axial Precession:
        Axial precession, a wobbling motion of Earth's axis, operates on a 26,000-year cycle. This motion changes the orientation of Earth's axis relative to its orbit, affecting the timing and intensity of seasons. The precession cycle contributes to long-term climate changes by altering the distribution of solar radiation throughout the year.
      - Eccentricity:
        Milankovitch cycles refer to variations in Earth's orbit and axial tilt that influence climate over long periods. Eccentricity, the shape of Earth's orbit, changes over a 100,000-year cycle. When the orbit is more elliptical, there are more significant variations in solar radiation, impacting climate. However, these changes occur gradually, leading to long-term shifts in climate patterns.