As I understand the data, the man made element of the present warming is superimposed on top of any natural warming.
The natural warming is thought to be less than 10% of the warming, and the man made (in the 20th century) 90 - 95%. this being from 1 - 1.1 degrees centigrade per year.
This increase is significant as it tends to have positive feedback, as the atmosphere warms it encourages more warming.
"The Earth's rotation is affected by several cyclical movements, two of which are
axial precession (the wobble of Earth’s axis) and
obliquity (the tilt of Earth’s axis). These natural variations occur over long timescales (tens of thousands to hundreds of thousands of years) and are part of a phenomenon known as Milankovitch cycles, which impact the distribution of solar energy received by the Earth and contribute to long-term climatic changes, such as ice ages and warm periods.
- Axial Precession: This occurs over a cycle of about 26,000 years. It affects the orientation of Earth's axis relative to its orbit, altering seasonal contrasts and the distribution of solar radiation between the hemispheres. 2. Obliquity: The tilt of Earth's axis changes with a cycle of about 41,000 years, influencing the severity of seasons. When the tilt increases, summers are warmer and winters are colder, enhancing seasonal contrasts."
"Greenhouse gases (GHGs) are atmospheric gases that trap heat and contribute to global warming by enhancing the greenhouse effect. Key GHGs include:
1. **Carbon Dioxide (CO₂)**: Mainly produced from burning fossil fuels, deforestation, and industrial processes, CO₂ is the most significant human-released greenhouse gas with a long atmospheric lifetime.
2. **Methane (CH₄)**: Emitted from agricultural activities, landfills, and natural gas production, methane is much more potent than CO₂, with a global warming potential (GWP) about 25 times greater, but it has a shorter atmospheric lifetime.
3. **Nitrous Oxide (N₂O)**: Released from agricultural practices and fossil fuel combustion, N₂O has a GWP approximately 298 times that of CO₂ and contributes to ozone depletion.
4. **Fluorinated Gases**: This group includes synthetic gases like HFCs and SF₆ used in industrial applications. They have extremely high GWPs but exist in smaller quantities and can persist for long periods.
Additional considerations include water vapor, the most abundant greenhouse gas influenced by temperature, and ground-level ozone, a potent greenhouse gas created from pollution reactions.
The rise in GHG concentrations due to human activities has intensified the greenhouse effect, causing significant climate changes, such as rising temperatures and sea levels. To combat global warming, substantial reductions in GHG emissions across various sectors are needed, alongside efforts to transition to renewable energy and adopt sustainable practices."