Palaeoclimatic data refers to the information about past climate conditions on Earth. Understanding past climates is essential for comprehending long-term climate change patterns, predicting future climatic trends, and studying the natural variability of the Earth’s climate system. The study of palaeoclimates relies on various sources of data, both direct and indirect, that allow scientists to reconstruct past temperature, precipitation, atmospheric composition, and other environmental parameters. These sources are broadly categorized into proxy records and historical records, with proxy records being the most significant for periods before human documentation. One of the primary sources of palaeoclimatic data is ice cores. Ice cores are long cylinders of ice drilled from glaciers and ice sheets in polar regions, such as Antarctica and Greenland. These ice layers accumulate over thousands of years, with each layer representing a single year or season of snowfall. Ice cores preserve a wide range of climatic information, including trapped air bubbles that contain ancient atmospheric gases like carbon dioxide and methane. By analyzing the concentration of these gases, scientists can infer past greenhouse gas levels and their correlation with global temperatures. Isotopic analysis of the water molecules in ice, specifically ratios of oxygen-18 to oxygen-16, also provides temperature proxies, as these ratios vary depending on the temperature at the time the snow fell.