Climate change is influenced not only by human activities but also by several natural drivers that operate on various spatial and temporal scales. These natural drivers are critical in understanding past climate variations and in distinguishing anthropogenic influences from natural variability. The primary natural drivers include solar variability, volcanic activity, ocean-atmosphere interactions, and internal climate feedbacks. Solar variability is one of the most significant natural drivers of climate change. The sun’s output is not constant; it undergoes periodic fluctuations, primarily due to the 11-year sunspot cycle, which affects the amount of solar radiation reaching the Earth. During periods of high sunspot activity, the sun emits slightly more energy, which can lead to a modest warming of the Earth’s surface. Conversely, during periods of low sunspot activity, such as the Maunder Minimum in the 17th century, reduced solar output has been associated with cooler climatic conditions. Long-term variations in the sun’s energy output, over decades to millennia, also contribute to significant climate shifts. Volcanic activity is another natural driver of climate change. Large volcanic eruptions inject enormous quantities of ash, sulfur dioxide, and other aerosols into the stratosphere, where they can remain suspended for months to years. These aerosols reflect incoming solar radiation back into space, reducing the amount of energy absorbed by the Earth’s surface and causing short-term cooling. Historical examples, such as the eruption of Mount Tambora in 1815, led to the “Year Without a Summer,” demonstrating the significant impact volcanic eruptions can have on regional and global climates. While volcanic effects are usually temporary, repeated eruptions over time can influence climate trends. Ocean-atmosphere interactions play a crucial role in natural climate variability. Phenomena such as El Niño and La Niña, collectively known as the El Niño-Southern Oscillation (ENSO), lead to large-scale changes in sea surface temperatures across the tropical Pacific Ocean. El Niño events are typically associated with warming in the central and eastern Pacific, which can influence weather patterns globally, including increased rainfall in some regions and droughts in others. La Niña, in contrast, often results in cooler ocean temperatures in the same regions and different precipitation patterns. Other oceanic cycles, such as the Pacific Decadal Oscillation