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Lecture Slides
Lecture Slides

... •The carbon footprint of food not eaten is 3.3 Gt of CO2(Eq), the third top emitter of CO2 (equivalent) after China and USA!! •The Water foot print of food waste is 250 km3 • 1.4 billion hectares of land was used to produce the wasted food… roughly 1/3 of the agriculture land area •Impacts on biodiv ...
Document
Document

... 4th Assessment Report ...
Tom Blaine, Ph.D. Associate Professor(315 KB
Tom Blaine, Ph.D. Associate Professor(315 KB

Chloro – floro –carbons
Chloro – floro –carbons

...  Ice age – time in the past when continental glaciers covered large parts of Earth’s surface  Global warming – a gradual increase in the temperature of Earth’s atmosphere ...
Climate Change: the key issues
Climate Change: the key issues

... manage to slow warming rather than prevent it, societies will have more time to adjust to the changes. It is true that the action taken so far, such as the Kyoto Protocol, will only have a marginal effect. The protocol’s authors have always described it as a first step. But even before it came into ...
Global Warming - Millersville University
Global Warming - Millersville University

... Most people believe that Carbon Dioxide is the most dangerous and important Greenhouse Gas, when in fact, water vapor has a larger effect on Global Warming. Water vapor is always present in the atmosphere. It is naturally released into the atmosphere by Evaporation. Water vapor is responsible for re ...
Anthropogenic Contributors to Climate Change - 5.3
Anthropogenic Contributors to Climate Change - 5.3

... Since the start of the Industrial Revolution, humans have engaged in a range of behaviors (e.g., burning fossil fuels as an energy source and deforestation) that have increased the release of carbon dioxide into the atmosphere. Scientific consensus is that these behaviors are interrupting the carbon ...
Global Warming Terms
Global Warming Terms

... between reservoirs, occur because of various chemical, physical, geological, and biological processes. The ocean contains the largest pool of carbon near the surface of the Earth, but most of that pool is not involved with rapid exchange with the atmosphere. ...
High resolution RCM simulation of eastern Mediterranean climate
High resolution RCM simulation of eastern Mediterranean climate

... Modern global climate change evaluations usually based on application of coupled atmosphere-ocean global climate models (AOGCM). Contemporary European AOGCM models are characterized by quite coarse (~200 km) space resolution, which precludes them from representing effects of small scale processes. D ...
Global Warming Delusions BE NOT AFRAID The popular
Global Warming Delusions BE NOT AFRAID The popular

... Global warming doesn't matter except to the extent that it will affect life--ours and that of all living things on Earth. And contrary to the latest news, the evidence that global warming will have serious effects on life is thin. Most evidence suggests the contrary. Case in point: This year's Unite ...
climate change
climate change

... • Over the last 20 years, the temperatures went beyond 36.5 degrees Celsius on over nine occasions, as opposed to only four such years in the two preceding decades starting 1967. • Rains in Bangalore have also turned unpredictable. The months of September &October are when the city receives the high ...
2. Summer Arctic Sea Ice Decline
2. Summer Arctic Sea Ice Decline

... Potential climate change impacts • Humanity’s greenhouse gas emissions are expected to lead to climatic changes in the 21st century and beyond. These changes will potentially have wide-ranging effects on the natural environment as well as on human societies and economies. Scientists have made estim ...
Greenhouse Effect
Greenhouse Effect

... The energy warms the Earth's surface, and as the temperature increases, the Earth radiates heat energy (infrared energy) back into the atmosphere. As this energy has a different wavelength to that coming from the sun, some is absorbed by gases in the atmosphere. As a result, the Earth's average surf ...
Climate Change
Climate Change

... currents in the ocean vary through time ...
Earth science league..
Earth science league..

... Avoiding Earth Tipping Points We can still avert dangerous climate change. However, we are currently on a warming trajectory that will leave our world irrevocably changed, far exceeding the 2°C mark. This gamble could propel us into completely uncharted waters, with unmanageable sea-level rise and a ...
DOC - Europa.eu
DOC - Europa.eu

... (F-gases). Emissions of F-gases, which have a warming effect up to 23,000 times more powerful than carbon dioxide, have risen by 60% since 1990, while all other greenhouse gases have been reduced. The proposed Regulation aims to reduce F-gas emissions by two-thirds of today's levels by 2030. It also ...
NYT article: Q and A about climate change
NYT article: Q and A about climate change

... 8. How much will the seas rise? The real question is not how high, but how fast. The ocean is rising at a rate of about a foot per century. That causes severe effects on coastlines, forcing governments and property owners to spend tens of billions of dollars fighting erosion. But if that rate contin ...
Contrarian views on Climate Change
Contrarian views on Climate Change

... human-caused warming of the Earth’s atmosphere, is seen by many as the foremost threat facing our world today. The UN has convened scientific experts from around the world to research, measure and gauge possible responses to what many warn as significant global changes due to warming of the planet’s ...
Climate Change - University of Tasmania
Climate Change - University of Tasmania

... so one might expect quick changes • But we have seen how massive the atmosphere is 5 x 1015 tonnes • The earth itself is 6 x 1021 tonnes • These numbers are so large they are difficult to comprehend, but the point is, it will take a long time to heat the Earth up and a long time for it to cool off a ...
Short Answers to Hard Questions about Climate Change
Short Answers to Hard Questions about Climate Change

... That is actually hard to say, which is one reason scientists are urging that emissions be cut; they want to limit the possibility of any worst-case scenario coming to pass. Perhaps the greatest fear is a collapse of food production, accompanied by escalating prices and mass starvation. Even with run ...
Climate Change - Harlem School District 122
Climate Change - Harlem School District 122

... from plants throughout the world Most importantly, seeds that make up most of the agricultural industry. No matter what, the seeds will be frozen ...
Global Warming - MrKremerScience.com
Global Warming - MrKremerScience.com

... • remember that many of the feedback mechanisms below are happening simultaneously • remember also that there may be long lag times (delays) between a cause and its effect, often of many decades or centuries • Oceans • absorb CO2 from the atmosphere • as they warm up, they release CO2 back into the ...
PP3(Ch21-44)Climate Change
PP3(Ch21-44)Climate Change

... Winter High & Summer Low ...
Wikipedia `Climate change mitigation`
Wikipedia `Climate change mitigation`

... do not address problems such as ocean acidification caused by these gases. Solar radiation management projects often have the advantage of speed. On the other hand, carbon dioxide removal projects seek to remove greenhouse gases from the atmosphere (e.g., fertilising the world’s oceans with iron), a ...
2
2

... have been done and to develop strategies for future work. Sustained observations allow scientists to detect climatic spatial patterns. For example, the figure opposite shows interdecadal change in land and sea surface temperatures. This figure is taken from the 1996 Intergovernmental Panel on 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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