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Sarah Friedland
Sarah Friedland

... have different needs, it is important that all nations of the world come together to contribute some solutions to this issues. The United Kingdom is playing a part in preventing global warming while still staying true to their own interests. The United Kingdom has participated in all major internati ...
Chapter 16 - Global Climate
Chapter 16 - Global Climate

... • Earth absorbs this energy and re-emits as longwave radiation (infrared, “heat”) • Greenhouse gases (CO2, CH4 H2O) in the atmosphere absorb infrared radiation • This natural process allows the Earth to maintain an average yearly temperature of about 150 C (600 F). ...
Slide 1
Slide 1

Climate is the average meteorological conditions—temperature
Climate is the average meteorological conditions—temperature

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Learning about past catastrophes from the present perturbation

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The trapped heat is warming up the Earth and causing global

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Environmental concerns:

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Evolution of the climate science

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GLOBAL WARMING IMPACTS IN MISSISSIPPI

... 50%  since  the  1970’s  and  is  expected  to  continue  to   than   any  time  over  the  past  800,000   ...
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PPT - Harvard University

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Climate Change Impacts

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Global Warming

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Viewing Guide - North Carolina Museum of Natural Sciences
Viewing Guide - North Carolina Museum of Natural Sciences

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Climate Change L6 - Nicole

... time, but the more recent changes are not considered natural changes in the climate. The ice age is an example of a natural change in climate over time. Today's changes are occurring faster and with greater magnitude than previous climate changes. ...
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Tackling Climate Change: The role of the engineer

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Eco-Footprints and Climate Cnange: The Perfect Moral Storm

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IPCC Fifth Assessment Report: Climate Change 2013/14
IPCC Fifth Assessment Report: Climate Change 2013/14

... Warming of the atmosphere and ocean system is unequivocal It is extremely likely that human influence has been the dominant cause of observed warming since 1950 It is likely (with medium confidence) that 1983—2013 was the warmest 30-year period for 1400 years. It is virtually certain the upper ocean ...
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Climate change

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Lecture #10 Global Climate Change

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The world is at a crossroads - Climate Justice in BC: Lessons for

... “Inuit are facing the beginning of a possible end of a way of life that has allowed us to thrive for millennia because of the climate changes caused by global warming…. What will be left of our culture if this comes to pass?” Sheila Watt-Cloutier International Chair for Inuit Circumpolar Council ...
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Human Influence on Weather

... destroy ozone very efficiently, used in many things in 20th century – Ozone “hole” is an area over the south pole where stratospheric ozone levels have drastically fallen – Atmospheric conditions (extreme cold, polar vortex) lead to efficient ozone destruction there ...
climate science
climate science

... Yes. Even though an increase of a few degrees in global average temperature does not sound like much, global average temperature during the last ice age was only about 4 to 5 °C (7 to 9 °F) colder than now. Global warming of just a few degrees will be associated with widespread changes in regional ...
Global Environmental Issues: A Case Study on Global Warming
Global Environmental Issues: A Case Study on Global Warming

... …refers to an increase in average global temperature, also called:  Climate ...
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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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