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climate change
climate change

... Migration is very complex to understand and always has a big impact. It can be successful when individuals and communities use migration to increase their resilience. Successful migration can be considered a necessary and positive adaptation strategy. However, migration, and in particular forced dis ...
Climate change and the northern Russian treeline zone
Climate change and the northern Russian treeline zone

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Evolution of the Southern Annular Mode during the past
Evolution of the Southern Annular Mode during the past

Latin America
Latin America

... a result of climate change (Rosenzweig et al., 1993) could lead to an increased risk of hunger for an additional 50 million people by the year 2050. Because most Latin American countries’ economies depend on agricultural productivity, the issue of regional variation in crop yields is very relevant f ...
Business Plan - Central Victorian Greenhouse Alliance
Business Plan - Central Victorian Greenhouse Alliance

... This publication may be of assistance to you, but the Central Victorian Greenhouse Alliance does not guarantee that the publication is without flaw of any kind or is wholly appropriate for your particular purposes and therefore disclaims all liability for any error, loss or other consequences which ...
Integrating Climate Change Adaptation into Coastal Zone Management
Integrating Climate Change Adaptation into Coastal Zone Management

... which depend on a healthy coastal environment. Policies to reduce greenhouse gases could lead to the development of alternative renewable energy sources some of which could be generated along the coast from tides, waves or wind. Much of the nation’s coastal resources have already been destroyed, dam ...
onp_draft_112011 - University of Washington
onp_draft_112011 - University of Washington

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CLIMATE CHANGE MONITORING REPORT 2013
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Sea-level Rise Projections
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Integrating biophysical models and evolutionary theory
Integrating biophysical models and evolutionary theory

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Peru-Chile upwelling dynamics under climate change - HAL-Insu
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... understanding, and in order to protect biodiversity, wild nature and coherent green areas are highlighted. Rich biodiversity is thus framed as a favorable state that is threatened by human agency. Although value-laden and normative, the biodiversity concept is also closely connected to science and s ...
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PDF - Climate Diplomacy

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A Climate of Concern: Climate Change and Health Strategy

... Toronto’s Health in a Changing Climate The evidence is clear, and it has been for some time. Climate change is a reality and it is already having an impact on our health. Whether our focus is on the creeping effects of gradual climate change or the unexpected and often violent effects of severe wea ...
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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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