Natural climate change processes
Natural Climate Change Processes
Solar Variations
- The Earth’s climate is significantly influenced by variations in solar radiation.
- Sunspots, dark patches on the Sun’s surface, can increase solar radiation, leading to warmer conditions on Earth.
- The Sun goes through cycles of high and low activity approximately every 11 years, influencing Earth’s climate.
Volcanic Activity
- Volcanoes emit large quantities of greenhouse gases and particulate matter.
- A significant eruption can cool the planet by blocking sunlight, known as a volcanic winter.
- However, the long-term climate effect of volcanic eruptions is typically a warming due to increased levels of greenhouse gases.
Planetary Movements
- Changes in Earth’s orbit (known as Milankovitch cycles) influence the amount of sunlight the planet receives and consequently its climate.
- The axial tilt of the Earth also varies over time affecting the severity of seasons.
- Precession, a change in the direction in the axis of rotation of the Earth, impacts global temperatures and seasonality as well.
Atmospheric Gas Concentrations
- The concentration of gases in the atmosphere, particularly carbon dioxide and methane, significantly influence our climate.
- These gases are part of the Earth’s natural greenhouse effect, trapping heat and maintaining a livable global temperature.
Oceanic Processes
- The thermal circulation of the oceans has a significant impact on climate by distributing heat around the globe.
- Phenomenon like El Niño and La Niña alter the distribution of warm and cold water in the Pacific, which can impact climate globally.
Bio-Geological Processes
- Living organisms, including humans, alter the climate through the release or capture of greenhouse gases.
- For example, plant growth and decay cycles can influence levels of carbon dioxide, and thus global temperatures.