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Impacts of global warming on arctic pelagic ecosystems and pelagic
Impacts of global warming on arctic pelagic ecosystems and pelagic

... THE ARCTIC has an important, but so far inadequately known role on the climate of the globe. Recent observational studies have revealed significant reductions in Arctic sea-ice cover and thickness and increased air and ocean temperatures, indicating that we may already be seeing the early warning si ...
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Climate Change: Law, Policy, and Business

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... additional black carbon (BC), emitted and hence deposited on snow and ice, could decrease albedo and speed up melting. A study led by researchers at the University of Leeds brought together Arctic shipping inventories for 2004, projected inventories for 2050 and a global aerosol model and found that ...
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Million Species

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Climate change feedback



Climate change feedback is important in the understanding of global warming because feedback processes may amplify or diminish the effect of each climate forcing, and so play an important part in determining the climate sensitivity and future climate state. Feedback in general is the process in which changing one quantity changes a second quantity, and the change in the second quantity in turn changes the first. Positive feedback amplifies the change in the first quantity while negative feedback reduces it.The term ""forcing"" means a change which may ""push"" the climate system in the direction of warming or cooling. An example of a climate forcing is increased atmospheric concentrations of greenhouse gases. By definition, forcings are external to the climate system while feedbacks are internal; in essence, feedbacks represent the internal processes of the system. Some feedbacks may act in relative isolation to the rest of the climate system; others may be tightly coupled; hence it may be difficult to tell just how much a particular process contributes. Forcings, feedbacks and the dynamics of the climate system determine how much and how fast the climate changes. The main positive feedback in global warming is the tendency of warming to increase the amount of water vapor in the atmosphere, which in turn leads to further warming. The main negative feedback comes from the Stefan–Boltzmann law, the amount of heat radiated from the Earth into space changes with the fourth power of the temperature of Earth's surface and atmosphere.Some observed and potential effects of global warming are positive feedbacks, which contribute directly to further global warming. The Intergovernmental Panel on Climate Change's (IPCC) Fourth Assessment Report states that ""Anthropogenic warming could lead to some effects that are abrupt or irreversible, depending upon the rate and magnitude of the climate change.""
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