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The Little Ice Age in Scientiªc Perspective: Cold
The Little Ice Age in Scientiªc Perspective: Cold

... arctica where recent temperatures are still ºuctuating below earlier levels, possibly reºecting effects of climate inertia from the surrounding oceans, although the causal mechanism is still uncertain.7 Focusing on the European Alps, at least two independent proxy archives—glaciers and tree rings—ex ...
Environmental Change: Adaptation Challenges
Environmental Change: Adaptation Challenges

... (EU Strategy on adaptation to climate change, Brussels, 16. 4. 2013, p. 216) This monograph summarizes theoretical and empirical evidence of environmental change impacts on the physical environment and human societies, with a focus on climate change. Global climate change is considered as one of the ...
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... PRINCIPAL FEATURES Purpose of Bill In order to contribute so far as is reasonably practicable to limiting the inevitable and harmful effects of global average temperature increases, to ensure that emissions of greenhouse gases in the State do not exceed the levels binding the State under European Un ...
Dr Manohar Arora
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... (UNFCCC) defines “climate change” as: ‘a change of climate which is attributed directly or indirectly to human activities that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over comparable time periods’ ...
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... rising in real terms over time, would be required to achieve. This yields kA = 1/6. ...
Links between Ozone and Climate
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... Atmospheric ozone is affected by climate change • Increases in CO2 cool the stratosphere Slows down the rate of gas-phase ozone destruction  O3 increase Tendency to increase loss in polar latitudes • Increase in GHGs changes the stratospheric circulation Changed circulation changes stratospheric o ...
Oxfam`s post COP21 analysis
Oxfam`s post COP21 analysis

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SoP_Letter submitted to HL Champions
SoP_Letter submitted to HL Champions

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Clemmitt, "Climate change"
Clemmitt, "Climate change"

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Ecuador`s Intended Nationally Determined Contribution
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... with oneself, with the rest of the community, with different cultures and with nature. It was under this premise that Ecuador established, by referendum, a new constitution in 2008 in Montecristi, which has been without a doubt a crucial step to addressing national and global issues. Our Constitutio ...
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Item 5 - Government Consultation On the Draft Climate Change Bill
Item 5 - Government Consultation On the Draft Climate Change Bill

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... need your leadership now more than ever to reduce the risks of a dangerously warming climate. The science is clear that human activity is the dominant cause of warming over the last half century.1 If global heat-trapping emissions continue to rise, the scope and severity of risks will accelerate. Al ...
Final review - UCLA: Atmospheric and Oceanic Sciences
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Developing and Applying Scenarios: A summary from the Third
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... climate, impacts and outcomes to describe the coping range. • Address adaptation to climate variability and extremes as part of reducing vulnerability to longer-term climate change. • Assess risk according to how far climate change, in conjunction with other drivers of change, may drive activities b ...
Expansion of the Hadley cell under global warming
Expansion of the Hadley cell under global warming

... warrants further investigation. [5] Here, we investigate the response of the HC to global warming using 21st century increasing GHG scenarios from the Fourth Assessment Report (AR4) of the Intergovernmental Panel on Climate Change (IPCC). The diversity of the numerical schemes and parameterizations ...
Global Systems - study guide notes
Global Systems - study guide notes

... the chlorine atom. This atom will react with ozone, breaking ozone into normal oxygen which does not block out the UV-b radiation. In the late 1980’s and international ban on CFC’s has slowly had a levelling off effect on the rate of ozone depletion. ...
Contribution of Greenhouse Gas Emissions
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... oxygen, argon, and trace gases whose concentration varies little over time and location. Other gases such as water vapor, sulphur dioxides, and nitrogen oxides can vary substantially over time and location depending on air circulation patterns, temperature gradients, land use practices, and industri ...
A Call to Action for Conserving Biological Diversity in the Face of
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... Literature reviews about biological diversity and climate change have generally ignored a major focus of climate-change policy—mitigation. Conservation professionals will generally support mitigation because it confronts root causes by, for example, reducing emissions of greenhouse gases, insulating ...
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ECOLOGY, POLLUTION AND ENVIRONMENTAL HEALTH

... century, with accelerated warming during the past two decades. There is new and stronger evidence that most of the warming over the last 50 years is attributable to human activities. Human activities have altered the chemical composition of the atmosphere through the buildup of greenhouse gases – pr ...
Tackling climate change at the local level
Tackling climate change at the local level

... development so as to reduce carbon dioxide (CO2) emissions arising from construction ...
Presentation - Copernicus.org
Presentation - Copernicus.org

... Simulations of present climate temperature and precipitation episodes for the Iberian Peninsula M.J. Carvalho, P. Melo-Gonçalves and A. Rocha CESAM and Department of Physics, University of Aveiro Correspond to [email protected] ...
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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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