Palaeoclimatic data refers to information about the Earth's past climate, which scientists use to understand long-term climate changes and patterns over millions of years. Since direct measurements of climate, such as temperature and rainfall, have only been recorded for a relatively short period in human history, researchers rely on indirect evidence preserved in natural archives. These records help reconstruct past climates and understand the processes influencing climate change. The sources of palaeoclimatic data are diverse, each providing unique insights into past environmental conditions. These sources can be broadly categorized into geological, biological, and chemical proxies, and each type offers a window into different aspects of the Earth's climate system. One major source of palaeoclimatic data is ice cores. Ice cores are cylindrical samples drilled from ice sheets and glaciers, primarily in Greenland and Antarctica. These cores contain layers of ice that have accumulated over hundreds of thousands of years. Each layer traps tiny bubbles of atmospheric gases, including carbon dioxide, methane, and nitrous oxide, which are crucial indicators of past greenhouse gas concentrations. By analyzing the isotopic composition of oxygen and hydrogen in the ice, scientists can estimate past temperatures and precipitation patterns. Additionally, ice cores may contain particles such as volcanic ash, dust, and pollen, which provide further information about past atmospheric conditions, volcanic activity, and vegetation changes. Ice cores have been