People and Planet - Scientists Use Feedback Loops

What are feedback loops? And what do scientists use them for? Are they some kind of bungie cord used to secure expensive  equipment? A nutritious doughnut? Straps through which corn belts are placed?

None of the above. Feedback loops happen when past outcomes of phenomenon influence the same phenomenon in the present or future. Scientists use feedback loops to inform the public about Earth’s interacting systems. Feedback loops are particularly helpful in understanding global warming as is illustrated in the following ABC news article: 

What is a “Feedback Loop”?
POINT BARROW, Alaska, Feb 18, 2006.

Scientists say the warm weather adds to global warming because of "feedback loops."

In a feedback loop, the rising temperature on the Earth changes the environment in ways that then create even more heat. Scientists consider feedback loops the single-biggest threat to civilization from global warming.

Past a certain point -- the tipping point, they say -- there may be no stopping the changes.

Scientists working in the Arctic report that feedback loops are already under way. As the frozen sea surface of the Arctic Ocean melts back, there's less white to reflect the sun's heat back into space -- and more dark, open water to absor that heat, which then melts the floating sea ice even faster. More than a third of summer sea ice disappeared in the past 30 years.

In the ground next to the ocean, scientists say, warming has also awakened another enormous danger -- billions of tons of carbon locked up for eons by what was once frozen ground.

"I feel very uncomfortable about it," says Walter Oechel, a scientist studying the problem. "I mean, it's not the way the Arctic should be."

Oechel discovered that as global warming thaws and dries out the vast tundra, old decayed vegetation releases carbon dioxide. That's the same greenhouse gas that comes from car and plane exhausts, and power-plant chimneys -- and the tundra releasing carbon dioxide warms the atmosphere even more.