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Insights into climate change feedback loops, focusing on the interactions between the atmosphere and ocean. It explains how global warming can lead to increased wind speeds, higher ocean waves, and the release of salt particles that act as cloud nuclei, resulting in larger clouds. The document also discusses the potential impact of these clouds on global temperatures, and categorizes the feedback mechanism as positive or negative.
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Student Sheet 1
Systems are made up of parts and the interactions between them. They are composed of: Storages of matter/energy : tree biomass in trunk & leaves. Flows: inputs & outputs : light, oxygen and heat. Processes which transfer or transform the energy/matter) : photosynthesis. Feedback loops: affecting the stability
To be stable, all systems need to be self-regulating. Feedback loops permit systems to adjust their response to change (forcing factors) to return to stable conditions. Systems diagrams contain boxes that show circles and arrows which indicate flows.
A feedback is similar to a cause and effect loop, where information about a system is sent back to the system to improve its performance. An example is your body's ability to control temperature. The condition of the body's temperature is the information fed back to the brain, which is the controller. If the temperature is high, the body sweats in order to cool down. Since the process of sweating is done to stop the temperature change, this is a negative feedback.
Feedback loops come in two flavors: positive and negative. A negative feedback loop reduces the effect of change and helps maintain balance. A positive feedback loop increases the effect of the change and produces instability. In this case, the positive and negative naming of the loops do not indicate whether the feedback is good or bad. In climate change, a feedback loop is something that speeds up or slows down a warming trend. A positive feedback accelerates a temperature rise, whereas a negative feedback slows it down.
Student Sheet 2
Scientists have identified several positive feedbacks loops in the climate system. Ocean warming provides a good example of a potential positive feedback mechanism. The oceans are an important sink for CO 2 through absorption of the gas into the water surface. As CO 2 increases, it increases the warming potential of the atmosphere. If air temperatures warm, it should warm the oceans. The ability of the ocean to remove CO 2 from the atmosphere decreases with increasing temperature. Because of this, increasing CO 2 in the atmosphere could have effects that actually intensify the increase in CO 2 in the atmosphere.
A good example of a negative feedback mechanism will be if the increase in temperature increases the amount of cloud cover. The increased cloud thickness or amount could reduce incoming solar radiation and limit warming. At the same time, it is not clear, that if additional cloud cover happens, at what latitudes and at what times it might occur. Also, it is not clear what types of clouds might be created. Thick low clouds would have a stronger ability to block sunlight than extensive high (cirrus) type clouds.
Various other feedbacks – related to emissions from soils and permafrost, for example, and changes to ocean evaporation – are known or thought to exist. Feedback loops such as these are very complex in themselves and even more complex when considered as part of an integrated global climate system. Some are already at work, while others have yet to kick in. Others still – both positive and negative – may yet be discovered.
Higher wind speeds Higher^ ocean^ waves
More salt particles released into air
Salt particles become nuclei for clouds
Bigger clouds
What effect?
GLOBAL WARMING
Heat energy
Higher atmospheric temperatures