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Videoconference Protocol
Videoconference Protocol

... seek solutions at the individual, institutional, and governmental levels and implement them at the local, regional and global scale. One of the most serious issues facing the world is global climate change. The general scientific consensus is that humans are increasing atmospheric levels of greenhou ...
Grantham Briefing Note 2 – September 2013 Climate sensitivity
Grantham Briefing Note 2 – September 2013 Climate sensitivity

... In addition to the two parameters above, AR5 also uses the near linear relationship between cumulative carbon dioxide emissions over time and global mean temperature change to define the Transient Climate Response to Cumulative Carbon Emissions (TCRE). TCRE provides a measure of transient global mea ...
Warming World Interactive
Warming World Interactive

... satellites and weather balloons show that the lowest layer of the atmosphere—where we live, airplanes fly, and weather occurs—is warming. Greenhouse gases are building up in this layer, trapping heat radiated from Earth's surface and raising the planet's temperature. Data ...
Warming World - Interactive
Warming World - Interactive

... satellites and weather balloons show that the lowest layer of the atmosphere—where we live, airplanes fly, and weather occurs—is warming. Greenhouse gases are building up in this layer, trapping heat radiated from Earth's surface and raising the planet's temperature. Data ...
Keith_Brander Iimpacts of climate change
Keith_Brander Iimpacts of climate change

... Marine ecosystems have always been affected by changes in climate at timescales from decades to millions of years. Since the industrial revolution in the 19th century the increase in greenhouse gases has caused an accelerating rise in global temperature whose effects on marine biota can now be detec ...
Lecture 4
Lecture 4

... Emissions (flow): 1 tonne C = 3,67 tonnes CO2 Concentration in atmosphere (stock): 1 Gt (=109 tonnes) C = 0,47 ppm (parts per million) ...
Use of climate data and information for EEA climate
Use of climate data and information for EEA climate

... • 2015 was nominally the warmest year on record, according to different near-surface temperature observational analyses with anomalies close to 1oC. • the decade 2006-2015 was between 0.83 and 0.89 oC warmer than the period 1850-1899 (pre-industrial) ...
Whitley-Binder_ClimateChgImpacts_w_notes
Whitley-Binder_ClimateChgImpacts_w_notes

... Loss could affect availability of this habitat for spawning, juvenile rearing, migratory and over-wintering stopovers, commercial ...
GCC - Mr. Davey`s Science!!!
GCC - Mr. Davey`s Science!!!

... • Water vapor = the most abundant greenhouse gas and contributes most to the greenhouse effect – Could increase cloudiness, which might slow global warming by reflecting more solar radiation back into space ...
AOSS_NRE_480_L10_Feedbacks_20100216
AOSS_NRE_480_L10_Feedbacks_20100216

... • That balance relies on water to exist in all three phases. – Too warm could run away to “greenhouse” – Too cold run away to “snowball” ice ...
Climate
Climate

... around the world (4) ...
The Forest Service Climate Change Performance Scorecard
The Forest Service Climate Change Performance Scorecard

... The Forest Service Climate Change Performance Scorecard Each national forest and grassland is expected to do seven of the following by 2015: ...
Climate change and mountain environments
Climate change and mountain environments

... like a down coat that keeps body heat from escaping into space. We need greenhouse gases, in fact without them the Earth would be a frozen wasteland. The problem is that things are getting out of balance. Human activities have increased greenhouse gases leading to global warming. Global average temp ...
Trenberth Italy0708-moved
Trenberth Italy0708-moved

... from increased atmospheric demand associated with warming. Even as rains have become heavier (more intense), so dry spells have also become longer. The two go hand in hand and relate to how precipitation changes: more intense but less frequent, and the amount changes less. After a certain point wher ...
Climate change - Marshland School
Climate change - Marshland School

... essentially two separate issues. The “ozone hole” refers to the destruction of a layer of ozone molecules found high in earths atmosphere. plants, oceans, and soil release and absorb large quantities of carbon dioxide of the part earths natural carbon cycle. ...
Climate change: evidence from natural sciences and
Climate change: evidence from natural sciences and

... at least one important crop was identified in a country where the GDP share of agriculture is greater than 5%, then vulnerability was ranked as “high.” In the case of low dependency on agriculture and a decrease in only one significant crop yield (or no decrease at all), vulnerability was ranked as ...
Which of the following are scientific statements?
Which of the following are scientific statements?

... The climate system does not reach equilibrium instantaneously Other processes can change the equilibrium temperature. ...
Are you Clear About Carbon? - Cornwall Development Company
Are you Clear About Carbon? - Cornwall Development Company

... CH4 is another naturally occurring gas, formed by microbes that break down organic matter in oxygenpoor environments. It remains in the atmosphere for 11-12 years and accounts for 8% of UK man-made GHG emissions. Globally as much as two thirds of methane originates from man-made sources, such as liv ...
Global Warming
Global Warming

... half degree F (0.2 to 0.3°C) over the past 25 years (the period with the most credible data). The warming has not been globally uniform. Some areas (including parts of the southeastern U.S.) have cooled. The recent warmth has been greatest over N. America and Eurasia between 40 and 70°N. Warming, as ...
Briefing to MT - CHARLIE-GIBBS MARINE PROTECTED AREA
Briefing to MT - CHARLIE-GIBBS MARINE PROTECTED AREA

... and impacts further and faster than currently documented. The majority of Arctic sea ice scientists declare that the Arctic sea ice is past its tipping pointi, the point at which change becomes selfperpetuating until an altogether different state is reached. NSIDC suggest that the North Pole may be ...
Climate Change and Alaskan Wetlands
Climate Change and Alaskan Wetlands

... More than forty percent of the land in Alaska is classified as a wetland or water of the U.S. Alaskan wetlands account for more than sixty percent of the nation’s total wetland ecosystems (Hall et al. 1994). Most of Alaska wetlands have been projected by several scientists to disappear before the en ...
Weather, Climate, and (Especially) Society
Weather, Climate, and (Especially) Society

... Decades of research by many of the world’s leading natural scientists have enormously improved our understanding of how the climate system works, including the complex interactions of the atmosphere, oceans, land surface, cryosphere, orbital mechanics, and solar activity. This work has established c ...
Climate Change Presentation Vocabulary
Climate Change Presentation Vocabulary

... changes to the landscape. The Oak Ridges Moraine is a geological formation created by a glacier. Global Warming: A continual rise in the average temperature of the earth. This occurs in the air and water at the earth’s surface. Greenhouse: It is a heated building with a glass roof and sides that is ...
Cato Institute Policy Analysis No. 307: The Consequences of Kyoto
Cato Institute Policy Analysis No. 307: The Consequences of Kyoto

... 2.3 percent per year. However, according to a climate model of the National Center for Atmospheric Research recently featured in Science, the Kyoto emission-control commitments would reduce mean planetary warming by a mere 0.19 degree Celsius over the next 50 years. If the costs of preventing additi ...
Climate Change and the Responsibility of Civil Society:
Climate Change and the Responsibility of Civil Society:

... fallibility, that: 1. Foreseeable global warming will have moderate and mixed (not only harmful but also helpful), not catastrophic, consequences for humanity–including the poor–and the rest of the world’s inhabitants. 2. Natural causes almost certainly account for a large majority of global warming ...
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Global warming



Global warming and climate change are terms for the observed century-scale rise in the average temperature of the Earth's climate system and its related effects.Multiple lines of scientific evidence show that the climate system is warming. Although the increase of near-surface atmospheric temperature is the measure of global warming often reported in the popular press, most of the additional energy stored in the climate system since 1970 has gone into ocean warming. The remainder has melted ice, and warmed the continents and atmosphere. Many of the observed changes since the 1950s are unprecedented over decades to millennia.Scientific understanding of global warming is increasing. The Intergovernmental Panel on Climate Change (IPCC) reported in 2014 that scientists were more than 95% certain that most of global warming is caused by increasing concentrations of greenhouse gases and other human (anthropogenic) activities. Climate model projections summarized in the report indicated that during the 21st century the global surface temperature is likely to rise a further 0.3 to 1.7 °C (0.5 to 3.1 °F) for their lowest emissions scenario using stringent mitigation and 2.6 to 4.8 °C (4.7 to 8.6 °F) for their highest. These findings have been recognized by the national science academies of the major industrialized nations.Future climate change and associated impacts will differ from region to region around the globe. Anticipated effects include warming global temperature, rising sea levels, changing precipitation, and expansion of deserts in the subtropics. Warming is expected to be greatest in the Arctic, with the continuing retreat of glaciers, permafrost and sea ice. Other likely changes include more frequent extreme weather events including heat waves, droughts, heavy rainfall, and heavy snowfall; ocean acidification; and species extinctions due to shifting temperature regimes. Effects significant to humans include the threat to food security from decreasing crop yields and the abandonment of populated areas due to flooding.Possible societal responses to global warming include mitigation by emissions reduction, adaptation to its effects, building systems resilient to its effects, and possible future climate engineering. Most countries are parties to the United Nations Framework Convention on Climate Change (UNFCCC),whose ultimate objective is to prevent dangerous anthropogenic climate change. The UNFCCC have adopted a range of policies designed to reduce greenhouse gas emissions and to assist in adaptation to global warming. Parties to the UNFCCC have agreed that deep cuts in emissions are required, and that future global warming should be limited to below 2.0 °C (3.6 °F) relative to the pre-industrial level.
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