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Modeling Earth`s Climate - National Science Teachers Association
Modeling Earth`s Climate - National Science Teachers Association

173736_INTRODUCTION 12-1-11
173736_INTRODUCTION 12-1-11

... human experience and apprehension of it, will have been significantly altered both by the process and direct effects of anthropogenic global warming as well as by our adaptations, mitigations and other responses to it. The only remaining question is the magnitude of the change and how disruptive it ...
1.3-Drivers-Impacts-Coastal-Resources-2012-07-12
1.3-Drivers-Impacts-Coastal-Resources-2012-07-12

...  Research since AR4 has suggested that dynamic processes, particularly the loss of shelf ice that buttresses outlet glaciers, can lead to more rapid loss of ice than melting of the top surface ice alone.  There is growing consensus in the science community that sea-level rise at the upper end of t ...
Ecology of Ecosystems
Ecology of Ecosystems

... climate change during and beyond the 21st century. Geographic ranges of many species have shifted toward the poles and up in elevation Most plant species cannot naturally shift their geographical ranges sufficiently fast to keep up with climate change. ...
Climate Compared: Public Opinion on Climate Change in the United
Climate Compared: Public Opinion on Climate Change in the United

... Two of the most prominent market-based policy options related to climate change have been carbon cap-and-trade and carbon taxes, having been debated extensively in both federal systems during the past decade. Neither federal government has adopted such policies, although some American states and Ca ...
Clouds Have Made Fools of Climate Modelers
Clouds Have Made Fools of Climate Modelers

... W/m2/C corresponds to no feedback. (This means if the temperature of the atmosphere were uniformly increased by 1 C and nothing else changed, the top of the atmosphere would radiate 3.3 W/m2 more radiation to space.) The feedback is observed to occur on shorter time scales in response to evaporation ...
Tentative Agenda DAY 1: Thursday, 30 April 2015
Tentative Agenda DAY 1: Thursday, 30 April 2015

... Presentation: Tim Stumhofer, Robert Bosch Foundation Revisiting debt-for-climate swaps as an alternative source of climate finance Open discussion ...
Holocene Interglacial
Holocene Interglacial

... the Northern Signature J.M. Schaefer, G.H Denton, M. Kaplan, A. Putnam, R.C. Finkel, D.J.A. Barrell, B.G. Andersen, R. Schwartz, A. Mackintosh, T. Chinn, and C. ...
Converted from D:\PCLTrans\Out\HR0481P2750.PCL
Converted from D:\PCLTrans\Out\HR0481P2750.PCL

... Recognizing Al Gore as the recipient of the 2007 Nobel Peace Prize. ...
Fisheries and Climate Change: the IPCC Second Assessment
Fisheries and Climate Change: the IPCC Second Assessment

... • Proj. is +11 - 77 cm by 2100; from thermal expansion & melting of ice. USNA*: +19” by 2100 • Regional variations due to wind and atmospheric pressure, ocean density, land motion, currents • Wetlands will decrease; sharply where there is shore protection • Higher wave energy; faster erosion *USNA= ...
climate wars, scientific evidence, and the future of homo sapiens
climate wars, scientific evidence, and the future of homo sapiens

... world deliberately misrepresent the work of their own colleagues? Why would they spread accusations with no basis? Why would they refuse to correct their arguments once they had been shown to be incorrect? And why would the press continue to quote them [doubters], year after year, even as their clai ...
Climate Truth File 2016
Climate Truth File 2016

... proponents don’t want to debate is what happened during a pivotal highprofile debate in 2007 in New York City, where skeptics were voted the clear winners against global warming proponents. NASA’s Gavin Schmidt appeared so demoralized at losing that debate that he announced debates equally split bet ...
Schmidt2007-Physics-of-ClimateModeling.pdf
Schmidt2007-Physics-of-ClimateModeling.pdf

... Climate projections made with sophisticated computer codes have informed the world’s policymakers about the potential dangers of anthropogenic interference with Earth’s climate system. Those codes purport to model a large part of the system. But what physics goes into the models, how are the models ...
Introduction to Climate Change Part II: Anthropogenic Climate Change
Introduction to Climate Change Part II: Anthropogenic Climate Change

... The atmosphere is changing ...
Support for climate policy and societal action are linked to
Support for climate policy and societal action are linked to

... certain that it is real and human caused, they recognize that it poses a serious threat to humans and that human action can reduce the threat, and they correctly understand that there is widespread agreement about climate change among scientists. Misunderstanding the widespread scientific agreement ...
Assessment of global warming on the island of Tenerife, Canary
Assessment of global warming on the island of Tenerife, Canary

... providing a worldwide network of observatories for monitoring the effects of global warming (Petit and Prudent 2008). At the same time, the higher mountainous islands are natural laboratories where such trends can be studied at different altitudes, from the marine boundary layer to the free troposph ...
Slide 1 - climateknowledge.org
Slide 1 - climateknowledge.org

... unrelated to CO2 – Need to think about time and balance here … • There are sources of T and CO2 variability other than the radiative greenhouse gas effect. – If CO2 increases in the atmosphere, there will be enhanced surface warming, but is the increase large enough to change temperature beyond othe ...
Preliminary preparatory meeting for next COP 23
Preliminary preparatory meeting for next COP 23

... organisation is the UNFCCC which was first drafted in 1992 and is now ratified by over 50 countries. Then the United Nations created the COP which is a governing body of an international convention, it has worked with the UNFCCC and the Kyoto protocol. The organisation has worked hard to create som ...
Slides of lection #4 (PowerPoint Presentation)
Slides of lection #4 (PowerPoint Presentation)

... Global warming… • Global temperatures could rise between 0.3 -6.4 degrees by ...
Global Climatic Mayhem
Global Climatic Mayhem

... Humanity is on the threshold.12 In biocentric, rather than anthropocentric, terms, life as we know it is on the threshold. The environmental system, in particular the earth’s climate, used to be regarded as relatively stable in the face of human insults. But now it is widely believed to have multipl ...
Climate Change
Climate Change

... The scattering of solar radiation cools the planet, while absorption of solar radiation by aerosols act to warm the air directly instead of allowing sunlight to be absorbed by the surface of the Earth. Aerosols have the ability to influence climate directly by absorbing or reflecting incoming solar ...
Meteorology-Climate - Onteora Central School District
Meteorology-Climate - Onteora Central School District

... How long would it take for the snow to reach a depth of 1,000 meters (m) if the average snowfall over an area of north central Canada is 100 centimeters (cm) per year? (Assume that there is no melting year round and no compaction of the ...
Globalization_CR - Department of Geological & Atmospheric
Globalization_CR - Department of Geological & Atmospheric

... There is a confidence level >66% that there will be an increase in droughts, tropical cyclones and extreme high tides. Both past and future anthropogenic carbon dioxide emissions will continue to contribute to warming and sea level rise for more than a millennium. Global atmospheric concentrations o ...
PDF
PDF

... ‘business as usual’ projection, global output of cereals will decline by between 0.7 per cent and 2.0 per cent, relative to the case of no change in climate, while the estimated change in agricultural GDP ranges from -1.5 per cent to +2.6 per cent. Darwin (1999) estimates that world welfare may incr ...
Climate-Change Projects—Selling of Indulgences or High Road?
Climate-Change Projects—Selling of Indulgences or High Road?

... the United Nations, and the voluntary carbon market is booming too. Lately, however, emissions trading has been criticized as the modern version of the buying and selling of indulgences. Yet it is a focal element of the entire climate-change policy. Prerequisites for the effective use of this instru ...
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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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