Answer:
A process seen as a good example of a positive feedback which then reaches a stable state in the Earth system can be depicted in ice - Albedo Feedback.
Explanation:
What are feedback in the first instance? - In terms of Earth system, they are processes that can either amplify or diminish the effects of climate <u>forcings</u>. They can be divided into positive and negative feedback.
Positive feedback increases the initial warming whereas, negative feedback does the opposite.
In the case of Ice - Albedo Feedback which happens to be a positive one, ice generally reflects sunlight better than any other material on earth and in so doing, the level of insolation absorbed by earth is lowered, thereby resulting to cooling. In this light, the increased cooling effect will result to the growth of more ice, thus, resulting to further insolation. This cooling favors more formation of ice and hence, promotes additional cooling. This cycle of increased cooling feeds back on itself to encourage the initial upset or change. As a result of this cycle, this case is referred to as a positive feedback.
NOTE: if positive feedback mechanism are left to its own devices, this will lead to a runaway cooling and perhaps a frozen earth. Therefore, positive feedback will generally trigger the negative feedback mechanism to annul its devastating effects if allowed.