Anthropogenic climate change refers to the alteration of the Earth’s climate system caused primarily by human activities such as the burning of fossil fuels, deforestation, industrialization, intensive agriculture, and large-scale land-use changes. These actions release greenhouse gases like carbon dioxide, methane, nitrous oxide, and chlorofluorocarbons, which intensify the greenhouse effect and lead to a measurable rise in global temperatures. The detection and attribution of climate change rely heavily on a range of indicators that reflect physical, biological, and socio-economic changes in the environment. These indicators serve as evidence to distinguish anthropogenic impacts from natural climate variability, providing scientists and policymakers with essential tools for assessing the scope and urgency of the issue. One of the most fundamental indicators is the rising global average surface temperature. Since the pre-industrial era, the Earth’s mean temperature has increased by approximately 1.1°C, with the last few decades being the warmest on record. The Intergovernmental Panel on Climate Change (IPCC) has consistently reported that this warming correlates closely with the rise in anthropogenic greenhouse gas emissions. Temperature records from both land and ocean surfaces show not only a long-term upward trend but also an increasing frequency of heatwaves, warmer nights, and shorter cold seasons. These temperature changes cannot be explained solely by natural drivers such as volcanic activity or solar variability; rather, they align closely with human-induced increases in greenhouse gases. Another key indicator is the concentration of greenhouse gases in the atmosphere. Measurements from ice cores provide long-term historical data, while modern monitoring stations like the Mauna Loa Observatory in Hawaii record current levels with high precision. Carbon dioxide concentrations have risen from pre-industrial levels of about 280 parts per million to over 420 parts per million today, marking the highest