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Slide 1 - GLISAclimate.org
Slide 1 - GLISAclimate.org

... – Feedbacks • Incremental • Arctic / Ocean ...
Wilkins Paul Wilkins English 1302 F Deezy September 30, 2014
Wilkins Paul Wilkins English 1302 F Deezy September 30, 2014

... 17.2(2012):14-22. In this article by Donald R. Prothero he addresses what is actually happening in reality due to the human caused behind Global Warming. In the article he talks about how the carbon levels have increased in the earth’s atmosphere and what it’s causing to happen in the world, such as ...
The Time Bomb: Climate Change - Poverty
The Time Bomb: Climate Change - Poverty

... Legal Frameworks in Climate Change ...
Climate Sensitivity - UW Atmospheric Sciences
Climate Sensitivity - UW Atmospheric Sciences

... • Climate forcing - uncertain, especially solar and aerosol forcing. • Heat storage - somewhat uncertain. • Climate sensitivity - also uncertain. No two of these are known with enough precision to usefully constrain uncertainty in the third, with the data available, although it is possible to fit th ...
Document
Document

... climate change • “Earth's climate system is unequivocally warming • “It is more than 90% certain that humans are causing it • “Our activities increase concentrations of greenhouse gases in the atmosphere, • “Burning fossil fuels, deforestation and similar activities are the main causes Source = ‘Cli ...
1 Parmesan et al. Suppl climate attribution in ecology pg
1 Parmesan et al. Suppl climate attribution in ecology pg

... Root, T.L., Price, J.T., Hall, K.R., Schneider, S.H., Rosenzweig, C. & Pounds, J.A. (2003). Fingerprints of global warming on wild animals and plants. Nature, 421, 57-60. Root, T.L., MacMynowski, D.P., Mastrandrea, M.D. & Schneider, S.H. (2005). Humanmodified temperatures induce species changes: Joi ...
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... should not exempt developing countries In 2008, President Bush declared that the U.S. would take action on its own to reduce its GHG emissions, ...
Chapter 10 Planetary Atmospheres What is an atmosphere? Earth`s
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IGBP - WCRP
IGBP - WCRP

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Session 28 Tragedy of the Commons: The Arctic
Session 28 Tragedy of the Commons: The Arctic

... reduction of four greenhouse gases (GHG) (carbon dioxide, methane,nitrous oxide, sulphur hexafluoride) and two groups of gases (hydrofluorocarbons andperfluorocarbons) produced by them, and all member countries give general commitments. Annex I countries agreed to reduce their collective greenhouse ...
PPT - unece
PPT - unece

... the global atmosphere and which is in addition to natural climate variability observed over comparable time periods. ...
3.2 St Pauls Climate Change assessment File
3.2 St Pauls Climate Change assessment File

... higher temperatures, more in the North Island than the South, (but still likely to be less than the global average) rising sea levels more frequent extreme weather events such as droughts (especially in the east of New Zealand) and floods a change in rainfall patterns - higher rainfall in the west a ...
www.dwt.com
www.dwt.com

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No Slide Title
No Slide Title

The Global Carbon Cycle
The Global Carbon Cycle

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The Global Threat of Climate Change
The Global Threat of Climate Change

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Global Change SyllabusFS600x
Global Change SyllabusFS600x

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What is Climate Change?
What is Climate Change?

... and Europe becoming relatively cooler. Even if this were to occur, it would take many years or decades because oceans move heat and cold much more slowly than the atmosphere. (Some ocean changes, however, such as the periodic warming of Pacific Ocean waters known as El Niño, may affect regional weat ...
Short-Lived Climate Pollutants
Short-Lived Climate Pollutants

... –  Energy efficiency, fuel switch - Coal (oil) to natural gas etc. ...
Presentación de PowerPoint
Presentación de PowerPoint

... • Climate change is an urgent matter. We need to act now. • Both mitigation and adaptation are needed to truly fight climate change and the threats it poses to humanity. • Rich countries must cut emissions by 30% by 2020 and 80% by 2050. • International cooperation on finance and technology transfer ...
Co-benefits Policy and Research beyond Paris
Co-benefits Policy and Research beyond Paris

... Article 3: As nationally determined contributions to the global response to climate change, all Parties are to undertake and communicate ambitious efforts... ...
Why this change? - The University of the West Indies at Mona
Why this change? - The University of the West Indies at Mona

Sustainability
Sustainability

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A guide to Representative Concentration Pathways
A guide to Representative Concentration Pathways

... the balance of energy that enters the atmosphere and the amount that is returned to space compared to the pre-industrial situation. Total radiative forcing is determined by both positive forcing from greenhouse gases and negative forcing from aerosols. The dominant factor by far is the positive forc ...
Ethiopia at a glance
Ethiopia at a glance

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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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