paleotemp

Paleotemp, short for paleotemperature, refers to the reconstruction of Earth's historical climate temperatures over geological timescales. Scientists analyze natural records such as ice cores, sediment layers, and fossilized remains to infer past temperature conditions. This information helps us understand how Earth's climate has changed over millions of years, providing insights into natural climate variability and guiding predictions of future climate trends. Paleotemp is essential for studying long-term climate patterns, understanding the effects of factors like ice ages, and assessing how current human activities may influence future global temperatures.