Kliimatõlitust

Kliimatõlitust refers to the ongoing and observable changes in Earth's climate patterns over extended periods. These changes are primarily driven by natural processes, but scientific consensus indicates that human activities have become a significant contributing factor, especially since the mid-20th century. The most prominent aspect of current kliimatõlitust is the warming of the planet's average temperature, often referred to as global warming.

Evidence for kliimatõlitust comes from various sources, including temperature records, melting glaciers and ice sheets, rising sea levels, and changes in precipitation patterns. These shifts can lead to a range of impacts, such as more frequent and intense extreme weather events like heatwaves, droughts, floods, and storms. Ecosystems are also affected, with consequences for biodiversity and agricultural productivity.

The scientific understanding of kliimatõlitust is based on extensive research and data analysis from numerous disciplines. While the term itself is a general description of climate variability, in contemporary discourse, it often emphasizes the human-induced component and its associated risks. Understanding and addressing kliimatõlitust is a major focus of international scientific and policy discussions, aiming to mitigate its causes and adapt to its effects.