15 Climate Feedback Loops and Examples
The cascading effects from climate change can have unforeseen consequences. These are the climate feedback loops that either amplify or reduce the effects of climate change.
Think of it like a domino effect:
In a positive feedback loop, an initial warming triggers a feedback to amplify the effects warming. Whereas negative feedback loops reduce the effects of climate change.
So once you begin taking climate out of its balance, these positive and negative feedback loops start to kick in. Then, they can go beyond our ability to control it.
Negative climate feedback loops
We’re changing Earth’s climate. What happens next?
Negative climate feedback loops have beneficial results.
Instead of continued warming, they spark a favorable chain of events that lessen the severity of climate change.
Here are examples of negative feedback mechanisms for climate change:
1 Increased cloudiness reflects more incoming solar radiation
As ice sheets melt, this could increase cloudiness with more water vapor in the atmosphere.
Because clouds reflect 1/3 of incoming solar radiation, there would be less heat absorption on Earth’s surface.
2 Higher rainfall from more moisture in the atmosphere
Similarly, if there’s more water held in atmosphere, then higher water volume leads to more precipitation. This is because the atmosphere can retain more moisture with higher temperatures. But the downside is that ocean circulation patterns would change and creates an imbalance of where rainfall occurs.
3 Net primary productivity increase
As higher concentrations of CO2 enter the atmosphere, plants have more material to photosynthesize. If you isolated a single plant in a laboratory, then the CO2 fertilization effect has some truth to it. But plants can’t grow indefinitely with rising CO2. This is because other factors like nitrogen. And if temperature rises, this can negatively influence plant growth.
4 Blackbody radiation
The energy released by Earth is a function of temperature. If Earth’s temperature increases, it raises the amount of outgoing radiation. So the more energy you add to Earth, then it will emit more energy. This concept is the Stefan-Boltzmann law which has an overall cooling effect.
5 Chemical weathering as a carbon dioxide sink
With more CO2 and water in the atmosphere, it increases carbonic acid which is just CO2 and water. Chemical weathering in rocks is a sink for atmospheric carbon dioxide. Thus, it weakens the greenhouse effect and leads to cooling.
6 The ocean’s solubility pump
The solubility pump refers to the ocean’s ability to transport carbon from its surface to the interior. The ocean serves an important role in regulating CO2 by dissolving it in water. As ice sheets melt, carbon storage increases. Currently, oceans absorb 33% of CO2 emitted to the atmosphere. Although this process cannot continue indefinitely, solubility pump efficiency depends on ocean circulation.
7 Lapse rate and altitude temperature
Lapse rate refers to the change of temperature with altitude. Air expands higher in the troposphere because there is less pressure. Conversely, air compresses lower in the troposphere because there is more pressure. Climate models indicate that global warming will reduce the decreasing rate of temperature with height. Overall, this weakens the strength of the greenhouse effect.
Positive climate feedback loops
Positive climate feedback loops accumulate to a more harmful result with increased heating.
By far, the bad outweighs the good for climate change scenarios.
At the top of the list, methane release is the most devastating.
It has the potential to cause a lethal chain reaction of atmospheric heating.
8 Permafrost melt sparks methane release
In the Arctic tundra, permafrost melt will trigger methane release in the atmosphere. Because methane is a more potent greenhouse gas than CO2. This type of positive feedback loop could be a tipping point for our climate. Currently, there’s only about 5 gigatons of methane in the atmosphere. But the amount of methane in the Arctic is in the hundreds of gigatons.
9 The removal of ice high albedo
Once the Arctic, Greenland and Antarctic ice sheets melt, water absorbs more heat. Because ice has a high albedo, it reflects 84% of incoming solar radiation. But once we remove our ice protective shield, water reflects as low as 5% of solar radiation.
10 Ocean circulation patterns disruption
Once ice melts in the Arctic, it will start shifting deep ocean circulation patterns in the Gulf Stream. Currently, this circulation pattern relies on heavy salt water from the north to transport warm water to Great Britain. Once ice sheets melt, it releases freshwater into the oceans. This disturbs this ocean conveyor belt by slowing down flow in the Atlantic Ocean.
11 Sea level rise
As the planet warms, ocean waters expand. Rising sea levels hit coastal cities the hardest. But another result will trigger further glacier calving. If you increase water volume, this could cause further chunks of ice to outpour into the oceans.
12 Rainforest drought and loss
Temperatures are projected to rise 2 to 6° by 2100. As a result of the warmer climate, this will result in larger evaporation losses. Despite the possibility of more rainfall, unpredictable weather may result in less soil moisture. Drought due to a warmer means the loss of some of the most productive place in world.
13 Wetland methane release
Wetlands are the largest natural source of methane in the world. Climate change is concerned with their health because heating can cause bogs to release methane. The amount of methane production is dependent on a number of factors. For example, soil temperature, oxygen availability and warmer environments all relate to climate change contributors.
14 More kindle for forest fires
Mid-latitude regions are poised to receive an imbalance in rainfall and increasing risk of drought. As a result, forest fires and desertification in forested region will lower their ability to be carbon sinks. Overall, this releases more carbon than forests can absorb into the atmosphere. Thus, this positive feedback loop causing further warming.
15 Gas hydrates in shallow water
In the shallow oceans, gas hydrates store enormous amounts of methane. They occur naturally throughout the world as forms of ice and methane. Because we find them in relatively shallow, they are particularly susceptible to warmer temperatures. And similar to melting permafrost, methane release is a potent greenhouse gas. Thus, it causes further global warming