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Climate, Carbon and Coral Reefs
Climate, Carbon and Coral Reefs

... Scientific research has unequivocally established that greenhouse gas emissions are leading to increasing changes in the Earth’s climate. In its Fourth Assessment Report, the Intergovernmental Panel on Climate Change, a body co-sponsored by the World Meteorological Organization and recipient of the ...
Climate change track in river floods in Europe
Climate change track in river floods in Europe

... was observed in the last two decades of the century, illustrating pronounced clustering of extreme events (Blöschl and Montanari, 2010). For Germany, Hattermann et al. (2013) showed that the results of change detection are far from being uniform over all parts of the country. In parts of Germany, ma ...
now - The City of Edinburgh Council
now - The City of Edinburgh Council

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Understanding the Forecast Second Edition David Archer d

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Silent but Deadly - Global Justice Now
Silent but Deadly - Global Justice Now

... with the reaction taking place at high temperature and pressure. Yara declares Scope 1 emissions via the Carbon Disclosure Project, although the most recent period for which data are available is the calendar year 2009. In that year, Yara's declared Scope 1 emissions were 12.5 million tonnes CO2e. N ...
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CLIMATE WORLDWIDE

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Outcome of Paris Climate Negotiations
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Apocalypse Nicked! - Geoengineering Governance Research
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Processes Responsible for Cloud Feedback
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Assessing the Effect of Rising Temperatures
Assessing the Effect of Rising Temperatures

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Indicator and data needs - Eionet Forum
Indicator and data needs - Eionet Forum

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Interactive comment on “Was the Little Ice Age more or less El Niño
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NASA faked the moon landing—therefore
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joint submission - The Internal Displacement Monitoring Centre
joint submission - The Internal Displacement Monitoring Centre

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A Summary of the Assessment Process of the Intergovernmental
A Summary of the Assessment Process of the Intergovernmental

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Climate and Atmosphere-- Bosnia and Herzegovina

... Protocol, which was adopted by consensus at the third session of the Conference of the Parties (COP-3) in December 1997, contains emission targets for Annex I (developed) countries for the post-2000 period. View full technical notes on-line at http://earthtrends.wri.org/searchable_db/variablenotes_s ...
Climate change impacts on water quality outcomes
Climate change impacts on water quality outcomes

... SedNet is a spatially distributed, time-averaged (decadal to century) model that routes sediment through the river network, based on a relatively simple physical representation of hillslope and channel processes at the reach scale, accounting for losses in water bodies (reservoirs, lakes) and deposi ...
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... Regulating water supply UNFCCC not considering adaptation aspect of forests Forests to be impacted by climate change ...
Trends and Variability in Snowmelt Runoff in the Western United
Trends and Variability in Snowmelt Runoff in the Western United

... timing could be related to the PDO, whereas Regonda et al. (2005) speculate that trends in SMR timing could be a response to the increased frequency of El Nino events in recent decades, or to general global warming. The first PC resulting from the PCA of the CMD data is not well correlated with eith ...
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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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