Paleoklimatologické
Paleoklimatologie is the scientific study of past climates. It seeks to understand climate conditions that existed prior to the widespread availability of instrumental records, typically before the mid-19th century. Paleoclimatologists use various natural archives, known as proxies, to reconstruct these ancient climates. These proxies include ice cores, which contain trapped air bubbles and isotopic signatures of past temperatures and atmospheric composition, as well as tree rings, which record annual growth variations influenced by climate. Sediments from ocean floors and lakebeds, fossilized pollen, and coral skeletons also provide valuable information about past temperature, precipitation, and environmental conditions. By analyzing these proxies, scientists can identify long-term climate trends, past climate events such as ice ages and periods of rapid warming, and the natural variability of Earth's climate system. This knowledge is crucial for understanding the causes of climate change, both natural and anthropogenic, and for improving future climate projections. Paleoklimatology helps contextualize current warming trends within the broader history of Earth's climate.