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Slide 1 - climateknowledge.org
Slide 1 - climateknowledge.org

... greenhouse gas produced by human activities Atmospheric CO2 has increased from a preindustrial value of about 280 parts per million (ppm) to 379 390 400 ppm in 2005 2010 2014 The atmospheric concentration of CO2 in 2005 2010 2014 exceeds by far the natural range (180 to 300 ppm) over the last 650,00 ...
FINAL EXAM: MONDAY MARCH 17 3-6PM
FINAL EXAM: MONDAY MARCH 17 3-6PM

... Weather: Atmospheric state at a particular time Climate: Weather averaged over many times (30 or more) ...
Unit 1 Hazards and Climate Change Past Questions
Unit 1 Hazards and Climate Change Past Questions

... b) Explain how physical factors lead to a range of hazard risks in the Philippines (15) 8a) Suggest reasons why the populations of different countries vary in their attitudes towards climate change. (10) b) Explain why the impacts of Global Warming are predicted to be uneven and unfair (15) Jan 2012 ...
Why should we be concerned
Why should we be concerned

... Rise in sea level – "The consequences would be catastrophic," said Jonathan Overpeck, director of the Institute for the Study of Planet Earth at the University of Arizona in Tucson. "Even with a small sea level rise, we're going to destroy whole nations and their cultures that have existed for thous ...
CC-regime-complex-0
CC-regime-complex-0

...  The US Senate Byrd–Hagel Resolution blocked implementation of the Kyoto Protocol  The US subsequently tried to address climate change through other fora, for instance by creating the Major Economies Forum in 2009  States have also engaged in regional efforts at cooperation ...
Changes in atmospheric composition directly affect many aspects of
Changes in atmospheric composition directly affect many aspects of

... been or are about to be launched. Multi-platform studies of atmospheric chemical processes have been conducted on an unprecedented scale. Global chemical transport models can now simulate with some success the distribution of key tropospheric chemical species, and are capable of simulating future gl ...
Printer-friendly version - Weconnect
Printer-friendly version - Weconnect

... Data availability: the availability of spatial data to represent the criterion or of data from which the criterion may be derived. Confidence: the level of confidence that the criterion will influence vulnerability. ...
Slide 1
Slide 1

... • Sea level – By end of century from end of 21C, 0.19-0.58 m ...
THE CONFERENCE OF COPENHAGEN -2010
THE CONFERENCE OF COPENHAGEN -2010

... according to which developed countries should, by 2020, reduce emissions by 70-85%. This was a highly ambitious project, which was rejected, as expected, from the United States and China, for different reasons on either side, causing a strong reaction of the poorest countries. The disagreements betw ...
the Cancun Communiqué
the Cancun Communiqué

Media Release
Media Release

... records, spanning the period 1960 to 2012, covering 812 marine, freshwater and dry-land plant and animal species from the UK, from plankton to plants, butterflies to birds and moths to mammals. The data represented three levels of the food chain, primary producers (such as flowering plants and algae ...
Why councils should act now | (ppt 2.5MB)
Why councils should act now | (ppt 2.5MB)

... • Cutting greenhouse gas emissions has additional benefits: ...
The Science and Politics of Climate Change Transcript
The Science and Politics of Climate Change Transcript

... 2000 as the observations. There’s three sets of observations. The three coloured lines. They all show a very similar average global temperature, there’s a little bit of uncertainty. And it’s important to understand that the climate models were started in 1900, and apart from the changes in greenhous ...
2. The Earth, biosphere, climate and Man
2. The Earth, biosphere, climate and Man

... The climate of the Earth is described in terms of the temperature at e.g. the Earths surface, the strength of the winds and ocean currents, the presence of clouds and precipitation, to name a few of its most important features. Weather as we experience it day after day is obviously related to climat ...
Fate of Mountain Glaciers in the Anthropocene
Fate of Mountain Glaciers in the Anthropocene

... The primary triggers for ice ages and inter-glacials are well understood to be changes in the astronomical parameters related to the motion of our planet within the solar system and natural feedback processes in the climate system. The time scales between these triggers are in the range of 10,000 ye ...
NASA Air Quality Applied Sciences Team (AQAST)
NASA Air Quality Applied Sciences Team (AQAST)

... • Global radiative equilibrium: Fin = Fout • Perturb greenhouse gases or aerosols ...
Stronger Evidence of Human Influence on Climate
Stronger Evidence of Human Influence on Climate

... and have a blanketing effect similar to that of the greenhouse gases. But because clouds also reflect solar radiation, they act to cool the surface. Though on average the two opposing effects offset one another to a large degree, the net global effect of clouds in our current climate, as determined ...
Weather - University of Arizona
Weather - University of Arizona

implications of global warming for agriculture in ontario
implications of global warming for agriculture in ontario

... 6 macro-climatic regions of Ontario. This information on yields is then used for a series of analyses dealing with different attributes of the agricultural system. Details on the analytical methods, data sources, and results are presented in LEG (1985; 1986), Smit et al. (1989), and Brklacich and Sm ...
Regionalkonferenz der Metropolregion Hamburg
Regionalkonferenz der Metropolregion Hamburg

... and transformed by the public media. • Climate science is in a post-normal phase (where interest-led utility is a significant driver, and less so “normal” curiosity) ...
More knowledge, less certainty
More knowledge, less certainty

... knowledge and understanding increase over time, uncertainty should decrease? But while our knowledge of certain factors does increase, so does our understanding of factors we previously did not account for or even recognize. ...
Statement of relevance to the NOAA climate science and services
Statement of relevance to the NOAA climate science and services

... processes that control the climate system’s response to radiative perturbations. We focus on coupled interactions between the atmospheric dynamics, large scale radiation, ocean circulation and the cryosphere recognizing the inherent inter-connectedness of the subcomponents of the climate system. We ...
Future Sea Level Rise Sources
Future Sea Level Rise Sources

... 2. the resulting greenhouse gas concentrations in the atmosphere, which depends on the various sources and sinks of the various gases, 3. the effect of the changed concentrations on the radiative forcing of the atmosphere, 4. the effect of this forcing on the climate, in particular on temperature an ...
Global Warming and Cyclones: a Vicious Cycle
Global Warming and Cyclones: a Vicious Cycle

... May 14, 2009 -- Global warming can change storm patterns. In turn, storms might help fuel global warming. A new study suggests that tropical cyclones shoot water high into the atmosphere. The result may be a small but significant contribution to the greenhouse effect. "The bottom line is that tropic ...
SC ESSAY - Complete Document (1) final public
SC ESSAY - Complete Document (1) final public

... change, they are talking about trends in the changes of temperature, precipitation, wind patterns, and other atmospheric conditions that occur over long periods of time. The most significant of these trends is global warming, which refers to the rise in average temperatures near the Earth’s surface. ...
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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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