climate feedback mechanisms

Climate feedback mechanisms are processes that amplify or diminish the effects of climate change. For example, when Earth warms, ice melts, reducing the reflective surface (albedo) and causing more heat absorption, which accelerates warming. Another example is increased atmospheric water vapor from higher temperatures, which traps more heat and further warms the planet. These feedbacks can create self-reinforcing cycles, making climate change faster and more intense. Understanding these mechanisms helps scientists predict future climate impacts and develop strategies to mitigate them.