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Paleoclimate Implications for Human-Made Climate Change
Paleoclimate Implications for Human-Made Climate Change

... Paleoclimate data help us assess climate sensitivity and potential human-made climate effects. We conclude that Earth in the warmest interglacial periods of the past million years was less than 1 C warmer than in the Holocene. Polar warmth in these interglacials and in the Pliocene does not imply t ...
Thailand_1 - Georgia Institute of Technology
Thailand_1 - Georgia Institute of Technology

Sensitivity of the Humboldt Current system to global warming: a
Sensitivity of the Humboldt Current system to global warming: a

... components (sardines, anchovies and marine birds) off Peru display significant variations at a wide range of temporal scales, from interannual ENSO-related variability to interdecadal variability in relation to the Pacific Decadal Oscillation occurring in the North Pacific. Given that climate change ...
Educating for optimism and hope in troubled times
Educating for optimism and hope in troubled times

... rich and powerful...Eco-imperialism is intolerant of the freedom and sovereignty of the other, be it other communities, other countries, or other species. Mitigation is thus primarily the responsibility of the richer countries that have contributed most to global warming. It requires that every elem ...
North East England Greenhouse Gas Emissions Baselines and
North East England Greenhouse Gas Emissions Baselines and

... • produced a comprehensive greenhouse gas emissions inventory for North East England ; • developed a regional tool to enable the region to monitor its emissions ; • produced emissions trajectories showing the impact of existing regional plans and strategies ; and • developed a methodology for th ...
pdf
pdf

... What Is Climate Change? Climate refers to long-term changes in patterns of temperature, precipitation, humidity, wind, and seasons. Climate varies by region but overall the earth’s climate has been warming. Global temperatures over both land and ocean surfaces have risen ~0.85°C (1.5°F) since 1880.2 ...
Climate, Climate Change Nuclear Power and the Alternatives
Climate, Climate Change Nuclear Power and the Alternatives

...  But ongoing anthropogenic emission of “greenhouse gases” is increasing the strength of the greenhouse, and this can be bad: bad: humanity is vulnerable to changes in climate. ...
- White Rose Research Online
- White Rose Research Online

Pattern scaling using ClimGen: monthly
Pattern scaling using ClimGen: monthly

... ensembles of simulations, but that the errors that would thus result from using PS are small compared with the many other uncertainties that exist in future climate scenarios. More recent assessments, facilitated by ensembles of individual and multiple models, confirm that PS can approximately emula ...
Combined biogeophysical and biogeochemical
Combined biogeophysical and biogeochemical

... Studies of the net effect of historical land cover change on global temperature have shown that biogeophysical and biogeochemical mechanisms are of the same order of magnitude (Matthews et al., 2004; Brovkin et al., 2006). Therefore, in order to quantifiy the impacts of large scale land cover change ...
Evaluation of Climate Mitigation Potential for Yeniçağa Gölü (Bolu
Evaluation of Climate Mitigation Potential for Yeniçağa Gölü (Bolu

... Change (IPCC), 2007). Even if the minimum predicted increase takes place, it will be larger than any century-long trend in the last 10,000 years (Intergovernmental Panel on Climate Change (IPCC), 2007). It is not only a threat to the biodiversity of the world but it is expected to cause other global ...
Oilsands and Climate Change
Oilsands and Climate Change

... than surface mining, yet it is expected to overtake mining as the main approach to oilsands production over the next decade. This shift will increase the overall intensity of GHG pollution from the oilsands industry. • From 1990 and 2009, the GHG pollution per barrel of oilsands fuel produced declin ...
Coastal Vulnerability Handout
Coastal Vulnerability Handout

... Current Global Predictions of Sea Level Rise ...
PDF
PDF

... widespread cooperation on an unprecedented level, they face great uncertainties, both in relation to the magnitude and severity of the impacts of climate change, and the costs of alternative mitigation strategies. Despite these uncertainties, the recognition that climate change is one of the most pr ...
A climatic basis for microrefugia: the influence of terrain on climate
A climatic basis for microrefugia: the influence of terrain on climate

... the free atmosphere, and drive local variation in air temperature and water balance: (1) cold air drainage, (2) elevation, and (3) slope and aspect effects. My objective is not to rigorously review the components of mountain climate [see (Geiger, 1965), (Barry, 1992) for a thorough treatment of this ...
Belanger OLLI week4 slides - Denver Climate Study Group
Belanger OLLI week4 slides - Denver Climate Study Group

... 2. MID-OCEAN SPREADING RATES SLOW DOWN •Less CO2 into the atmosphere for volcanoes ...
The Intergovernmental Panel on Climate Change (IPCC) Why the
The Intergovernmental Panel on Climate Change (IPCC) Why the

... ❐ The IPCC’s First Assessment Report was released in 1990 and confirmed the scientific basis for concern about climate change. This lead to the decision by the UN General Assembly to prepare a UN Framework Convention on Climate Change (UNFCCC). The Convention entered into force in March 1994. ❐ The ...
Climate Change and the Past, Present and Future of Biotic Interactions
Climate Change and the Past, Present and Future of Biotic Interactions

... climatic change, and both modern and fossil evidence shows that disrupting their trophic interactions can amplify climate changes throughout the community (6, 9, 47). At the same time, experiments in aquatic systems show that warming can intensify trophic cascades, leading to stronger control by top ...
Here - Hydrol. Earth Syst. Sci.
Here - Hydrol. Earth Syst. Sci.

... The concern regarding water resources in the Andes is reflective of the rapidly changing climate throughout the region. This is most notable in observations of near-surface temperature, which show an increase of 0.7 ◦ C over the past seven decades (1939–2006, Vuille et al., 2008). Of the last 20 yea ...
Regional climate model data used within the SWURVE project
Regional climate model data used within the SWURVE project

... follow different storylines with respect to technological and economic growth in the world. The A2 storyline describes a heterogeneous world with strengthening of regional cultural identities, high population growth but with less concern for rapid economic development (Nakicenovic, 2000). The B2 sto ...
Impact of Climate Changes on Economic and Agricultural Value
Impact of Climate Changes on Economic and Agricultural Value

... GDP. Hence, it can be anticipated that developing countries will suffer more in the changing environment. The production of agricultural products is affected by higher temperatures, heat waves, changing weather patterns and high carbon dioxide levels in the atmosphere. However, the effect of these f ...
Projected changes in mean and extreme precipitation in Africa
Projected changes in mean and extreme precipitation in Africa

... Observed twentieth century precipitation used in this study was taken from the CRU TS2.1 gridded station data. Unlike in SHO09, dearth of station observations in the Global Historical Climatology Network (GHCN) data precluded delineating homogenous rainfall zones. For this reason, the climate zones ...
Inter American Institute for Global Change Research
Inter American Institute for Global Change Research

Geography at Key Stage 3. What will I learn? How will I be assessed
Geography at Key Stage 3. What will I learn? How will I be assessed

... Geography at Key Stage Four. What will I learn? How is this assessed? Autumn Term ...
Impact of Climate Change on Irrigation Demand and Crop Growth in a Mediterranean Environment of Turkey
Impact of Climate Change on Irrigation Demand and Crop Growth in a Mediterranean Environment of Turkey

... Crop growth was simulated using the detailed crop growth sub-model of the SWAP with a daily time step from sowing to maturity, based on eco-physiological processes that describe daily phenological development and growth in response to environmental factors such as soil and climate, and crop manageme ...
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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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