Understanding Feedback Loops: Temperature and Forest Area

In summary, the conversation discusses two feedback loops involving different variables and their interactions. The first loop involves solar heating, temperature, evaporation, and albedo, and is generally a negative feedback loop. The second loop involves forest area, plant evapotranspiration, rainfall, and is generally a positive feedback loop. The conversation also mentions the role of water vapor as a greenhouse gas and its potential impact on the loops.
  • #1
TheMathNoob
189
4

Homework Statement


I am just wondering if my analysis of the following feedback loops are right.

The invariant in this case is Temperature
Solar heating->Temperature->Evaporation cloud cover-> albedo->Solar heating
Second feedback loop

Invariant forest area
Forest area->Plant evapotranspiration and raincloud->rainfall->forest area

Homework Equations

The Attempt at a Solution



Temperature->evaporation cloud cover, it would be a positive coupling hence if more temperature, then more evaporation and cloud cover

Evaporation cloud cover-> albedo, Evaporation is a greenhouse gas , but at the same time it helps clouds form, so I will go with the greenhouse gas trait because evaporation is one of the causes of greenhouse gases. The coupling would be negative

Albedo->solar heating, if the albedo decreases then there would be more solar heating coming to the earth
, so it would be a negative coupling.

solar heating-> Temperature, positive coupling because if more solar heating coming to the Earth then more temperature

Generally it would be a a positive feedback loop

second feedback loop

Forest area-> plant evapotranspiration and raincloud, if the forest area increases then there would be more plants evapotranspirating and more raincloud

Plant evapotranspiration->rainfall, if there is more evapotranspiration and rain cloud then there would be more rainfall hence the vapor condenses and then it produces rainfall

rainfall->Forest Area, this one is tricky, assuming that the process is giving naturally then rainfall will help the forest area to protect from sunlight, so it would be positive coupling

generally it would a positive feedback loop
 
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  • #2
I think the first loop would be negative, because it has albedo as a link. To the extent that evaporation creates clouds, that increases albedo and - other things equal (which they won't be) - reduces solar heating.

The thing that at least partially offsets this is a different loop, with positive feedback, which is of the form:

Solar heating->Temperature->Evaporation-> Increased water vapour in non-cloud covered areas->Solar heating

In this case the water vapour acts purely as a greenhouse gas, which increases heating, because in those areas it has not formed clouds and hence does not generate the white surface needed for albedo.

Of course neither of these water-vapour-focused loops deal with the really important greenhouse gas CO2, which has other feedback loops (eg melting of permafrost releasing ground-stored CO2 into the atmosphere).
 

1. How do temperature and forest area affect each other?

The relationship between temperature and forest area is a classic example of a feedback loop. As temperature rises, it can cause a decrease in forest area due to factors such as increased evaporation and decreased plant growth. This decrease in forest area then leads to a decrease in carbon dioxide absorption and an increase in atmospheric carbon dioxide levels, which in turn contributes to further temperature increase. This vicious cycle continues until a new balance is reached.

2. How does deforestation impact temperature?

Deforestation, or the clearing of trees, has a significant impact on temperature. Trees play a crucial role in regulating temperature through the process of transpiration, where they release water vapor into the atmosphere. This water vapor cools the air and helps to maintain a stable temperature. Deforestation disrupts this process, leading to higher temperatures in the surrounding area.

3. What is an example of a positive feedback loop between temperature and forest area?

A positive feedback loop occurs when a change in one variable leads to a further increase or decrease in that same variable. In the case of temperature and forest area, a positive feedback loop could occur if rising temperatures cause trees to release more moisture, which then leads to a decrease in forest area and further temperature increase. This scenario would continue until a new equilibrium is reached.

4. How can we break the feedback loop between temperature and forest area?

Breaking the feedback loop between temperature and forest area requires a multifaceted approach. One solution is to reduce human-induced climate change by decreasing carbon emissions. Additionally, implementing sustainable forestry practices and reforestation efforts can help to increase forest area and mitigate the effects of rising temperatures. It is also essential to address the underlying causes of deforestation, such as agricultural expansion and illegal logging.

5. How can understanding feedback loops help us address issues related to temperature and forest area?

Understanding feedback loops is crucial in addressing issues related to temperature and forest area because it allows us to identify the root causes of these issues. By understanding the relationship between temperature and forest area, we can develop effective strategies to break the feedback loop and mitigate the effects of rising temperatures on forests. Furthermore, understanding feedback loops can help us anticipate and prevent potential future consequences of climate change, such as extreme weather events and biodiversity loss.

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