Climate change is being accelerated by its own effects. These are referred to as positive feedback loops. Here's why:
In climate change, a feedback loop is the equivalent of a vicious – or virtuous – circle. It's something that accelerates or decelerates a warming trend. A positive feedback accelerates a temperature rise, and a negative feedback decelerates it.
From the National Oceanic and Atmospheric Administration's (NOAA) National Climatic Data Center:
A
positive feedback is a process in which an initial change will bring about an
additional change in the same direction... There are also negative feedbacks,
processes in which an initial change will bring about an additional change in
the opposite direction.
It is
positive, rather than negative feedbacks that contribute to abrupt climate
changes. In positive feedbacks, a small initial perturbation can yield a large
change. Negative feedbacks, on the other hand, stabilize the system by bringing
it back to its original state.
A simple and obvious example of a positive feedback loop is melting polar ice. Polar ice is white(-ish) and it reflects back into space lots of sunlight. Polar ice has been melting as you know, and uncovering darker water or land underneath. Solar energy is then absorbed, instead of reflected, and so warming occurs, driving more polar ice melt.
It's a vicious circle, a feedback loop. It's positive (in scientific terms) because it is consisting in or characterized by the presence of something (increased temperature) rather than its absence (absence would be negative, i.e., cooling).
In general terms, there are three kinds of feedback loops
- ice-related feedback loops,
- vegetation-related feedback loops and
- feedback loops created by these that include larger influences, like ocean currents (the thermohaline circulation, e.g., the Gulf Stream) and air currents like the jet stream and events like El Ninos and El Ninas
Ice-related
- Methane hydrates – methane is a super-powerful greenhouse gas surfacing from the Arctic Ocean
- Siberian methane
- Darkening ice in Greenland
- Cracking glaciers release CO2
- Release of methane in the Antarctic
- Greatly accelerated Antarctic ice melt
- Darkening of ice caused by surface meltwater
- Amazon drought triggered the release of more methane than the US in 2010
- Decomposing peat in boreal forests
- Invasive growth warming soil and thus destabilizing permafrost
- Forest and bog fires burning at a rate greater than the last 10,000 years
- Thawing permafrost exposed to sunlight increases bacteria, leading to accelerated thawing
- Microbes as a contributor within thawing permafrost
- Warm seawater from the Atlantic ocean further warming the Arctic
- Canadian floodwater runoff
- Breakdown of ocean currents like the Gulf Stream
- Jet stream impacted by reduced temperature range between the poles and the equator
Next time: How bad might it get?
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