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Inquiry into The Kyoto Protocol
Inquiry into The Kyoto Protocol

... It is important to note that not all areas of the globe have warmed over the past few decades and these include parts of the Southern Hemisphere oceans and parts of Antarctica. Key conclusions from the TAR with regard to projected warming are: • The globally averaged surface temperature is projected ...
U.K. Rolls Out Carbon Trading for Businesses
U.K. Rolls Out Carbon Trading for Businesses

... One estimate is that the scheme will result in savings of about ₤1 billion (~ $1.5 billion USD) and a reduction of 4.4 million tons of CO2 per year by 2020. The U.K. seems to be on the forefront of carbon trading programs, first with its own Emissions Trading Scheme that predated the EU's and now wi ...
Hot, Flat & Dangerous
Hot, Flat & Dangerous

... ◦ Melting permafrost releases methane, 21x>CO2 ◦ Snow & ice melts = less reflection = raising ocean temp’s ◦ Ocean absorbs more CO2, raising acidity, harming food chain ...
09_climate change
09_climate change

... clearly continuing. Be careful of cherry-picking, and weather. Next slide ...
Download the paper
Download the paper

... temperature changes over the past 120 years (Figure 4). The Intergovernmental Panel on Climate Change (IPCC) has assembled a group of hundreds of climate scientists to assess the causes of the recent warming trends. Using a variety of tools, including well documented global circulation models, they ...
Pacific Northwest Climate Variability and Change
Pacific Northwest Climate Variability and Change

... – Appear to be higher than any time in past ~ 23 million yrs • The human footprint – Human activities altering the climate system – Human systems based on expectation of certain climate conditions – Population growth, political boundaries, resource dependency/depletion, habitat fragmentation limit a ...
28. 24 April
28. 24 April

... 24 April 2014 – Geog 3601 Lecture Summary 1. Paleoclimatology Datasets Continued our discussion of this web site: www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets and the handouts Tables 1.1 and 1.2. My expectation is that you become educated on any two datasets. Specifically: - Summary ...
Global Warming and Climate Impacts in Southern Africa
Global Warming and Climate Impacts in Southern Africa

... therefore, becomes imperative to study present and future trends associated with irrigation practices, that is, the depletion of surface and underground water. In addition, irrigation of large tracts of land may lead to the uprooting of local people from their traditional lands in addition to adver ...
FACTS ABOUT CLIMATE CHANGE
FACTS ABOUT CLIMATE CHANGE

... Earth’s climate changes naturally. Changes in the intensity of sunlight reaching the earth cause cycles of warming and cooling that have been a regular feature of the Earth's climatic history. Some of these solar cycles - like the four glacial-interglacial swings during the past 400,000 years - exte ...
Extracts from: Impact of climate change on agriculture in Africa by
Extracts from: Impact of climate change on agriculture in Africa by

... Concerns about climate change are global and real. As all communities try to get adapted to the challenges of their local climate, they are today sensitive to its variations. Third World countries, particularly Africa are threatened by the predicted effects of climate change because of their economi ...
Racing Extinction – The Warming Planet
Racing Extinction – The Warming Planet

... • Provide evidence to support your example, relating the example to extinctions today. ...
Dynamics of Climate Change slides
Dynamics of Climate Change slides

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Mr Philippe OMONDI
Mr Philippe OMONDI

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Gould - University of Hartford`s Academic Web Server
Gould - University of Hartford`s Academic Web Server

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Anthropogenic Climate Change_What Science tells About
Anthropogenic Climate Change_What Science tells About

... Feedbacks as solar forcing warms Earth: Decomposition releases greenhouse gasses: melting permafrost releases huge amounts of CO2 and methane. ...
Videoconference Protocol
Videoconference Protocol

... This semester we have discussed many of the issues that currently afflict our world and that make our current use of global resources unsustainable. We have learned that truly sustainable solutions address the complexity of these problems by considering the environmental, sociological, and economic ...
climate change and the greenhouse effect
climate change and the greenhouse effect

... easier not to think about climate change or take action, what would you say to them? I agree that it is an overwhelming topic but climate change affects all our lives from our water resources and public ...
Chapter 2 Climate Change: Scientific Basis
Chapter 2 Climate Change: Scientific Basis

... electricity. Coal accounts for 70% of electricity generation in Israel and 20% from natural gas, diesel fuel and fuel oil (2007 data). A wider use of natural gas is planned in the next couple of years, with an expected 35-40% of the electricity economy by 2025.15 In addition, the National Infrastruc ...
CLIMATE CHANGE: MYTHS AND REALITIES
CLIMATE CHANGE: MYTHS AND REALITIES

... to warm the planet for many decades if not centuries. Right now, there is about 40 percent more carbon dioxide in the atmosphere than there was at the dawn of the Industrial Revolution. The CO2 concentration is projected to reach twice the preindustrial level by the middle of this century. This doub ...
A Temperate Empire - Rachel Carson Center for Environment and
A Temperate Empire - Rachel Carson Center for Environment and

... least of all in terms of the weather. Farmers learned to cope with such differences by adapting to local conditions. For local and imperial elites, however, the environment proved to be more problematic and a persistent source of anxiety. They worried that widespread reports about its harshness woul ...
Chapter 9 Notes
Chapter 9 Notes

...  A rise in the average temperature of the earth, primarily caused ...
Climate Change in New York Recent Trends and Future
Climate Change in New York Recent Trends and Future

... Key Climate and Impacts Findings • Changes consistent with global warming are already evident across New York • Over next few decades, changes similar under both emissions scenarios • By mid-century, most changes are greater under the higher scenario • By late-century, under the higher scenario man ...
ppt - Department of Statistics | Rajshahi University
ppt - Department of Statistics | Rajshahi University

... global tropical storm days (1965–2008”).Geophysical Research Letters, 37, analyses the impact of the rising sea surface temperature (SST) on tropical cyclone (TC) activity is one of the great societal and scientific concerns. With the observed warming of the tropics of around 0.5°C over the past 4 t ...
Professor Neville Nicholls Presentation from the March
Professor Neville Nicholls Presentation from the March

... • In the last nine years, annual rainfall in the Murray Darling Basin (the “breadbowl” of Australia) the rainfall has been below 500mm. Prior to the current dry period, the longest period of below 500mm was six years. ...
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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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