Final answer:
The process described is an example of a positive feedback mechanism because it represents a cycle where an initial warming leads to further ice melt, which in turn increases heat absorption and accelerates global warming.
Step-by-step explanation:
The accelerating melt of summer sea ice and glaciers in the Arctic due to rising temperatures, which leads to darker-colored surfaces replacing lighter ones, thus increasing absorption and surface heating, is an example of a positive feedback mechanism in climate change. Positive feedbacks in the climate system lead to a cycle where an initial change is amplified by the reactions it causes, such as the reduction of ice, which decreases surface reflectivity, leading to more heat absorption and further warming.