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Observed climate variability and change
Observed climate variability and change

... the influence of human activities. Finally, there is emerging evidence for significant, rapid (time-scales of several decades or more), regional temperature changes during the last 10 000 years, well before the period for which anthropogenic influences could have been important (Fig. 2.24 of Chapter ...
Summary of Downscaling Methods
Summary of Downscaling Methods

... and usually used to produce time series (e.g., daily) of a climate variable or sets of climate variables (precipitation, temperature, solar radiation) • Parameters of weather generator are then conditioned on large scale predictors, such as the NAO or ENSO. ...
Objective of Downscaling
Objective of Downscaling

... and usually used to produce time series (e.g., daily) of a climate variable or sets of climate variables (precipitation, temperature, solar radiation) • Parameters of weather generator are then conditioned on large scale predictors, such as the NAO or ENSO. ...
Slowing anthropomorphic climate change
Slowing anthropomorphic climate change

... current mitigation technologies, leading to the invention and dissemination of new zero and low-carbon technologies and enhancing the capacity of countries to reduce their emissions. The United States and China are two of the world’s largest investors in clean energy and already have a robust progra ...
Global Climate Change AND Tropical Forest Ecosystems Andes
Global Climate Change AND Tropical Forest Ecosystems Andes

... (2008). Climate regulation of fire emissions and deforestation in equatorial Asia. Proceedings of the National Academy of Sciences 105 (51): 20350-20355. White, A., Cannell, M.G.R. and Friend, A.D., (1999). Climate change impacts on ecosystems and the terrestrial carbon sink: a new assessment. Glob ...
document
document

... terraces and strand lines can be seen to be exposed at a considerable height. ...
PDF
PDF

... many scientists believe the risks of negative impacts felt through global warming are substantial and suggest that society turn its attention to emission reduction. Emissions might, for example, be reduced through a new market mechanism to buy and sell emission permits, and by other means. Why might ...
Anopheles gambiae
Anopheles gambiae

... 160,000 deaths due to climate change in 2000 ...
Recent and future changes in the global and UK climate: high-res (2 MB) (opens in new window)
Recent and future changes in the global and UK climate: high-res (2 MB) (opens in new window)

... which begin in 1910. The average annual UK temperature increased by about 0.589°C between 1910-1939 and 1983-2012, and the seven warmest years on record have all occurred since 2000. Total annual rainfall has also been increasing since about 1970, and six of the ten wettest years on record have all ...
Centre for Environmental Rights
Centre for Environmental Rights

... emissions and reduction targets of the signatories to the UN Climate Change Convention are insufficient to realise the 2° target and therefore the chances of dangerous climate change should be considered as very high … the State is obliged to take measures in its own territory to prevent dangerous c ...
St. Francis Xavier University Thermoregulation
St. Francis Xavier University Thermoregulation

... processes. They may have an insulating layer of fat in the hypodermis of the skin. Fur and feathers also provide insulation. Endothermic animals can colonize a wide range of habitats. ...
10 Things To Know About The UN Climate Talks In Paris
10 Things To Know About The UN Climate Talks In Paris

... We’ll be talking about COPs, so it will be helpful to know some of that history. The following is from Wikipedia, which actually does a very good job of summarizing this. The United Nations Framework Convention on Global warming (UNFCCC) is an international environmental treaty negotiated at the Ear ...
Climate Change - Ev-K2-CNR
Climate Change - Ev-K2-CNR

... • Scientific research on forests, biodiversity and ...
US Climate Change Policy: Where Next? DiSCUSSioN PaPer
US Climate Change Policy: Where Next? DiSCUSSioN PaPer

... days for comment. It has been written as a result of legislation passed in December 2007 (during the Bush administration) that requires the introduction of a US-wide GHG emissions registry and that covers 85–90% of US emissions. In summary, the Rule proposes that suppliers of fossil fuels or industr ...
news and views - Victoria University of Wellington
news and views - Victoria University of Wellington

... As to the future, it is now clear that landsurface and ocean temperatures are rising in response to human-induced emissions of greenhouse gases — and remarkably fast on a geological timescale. The present concentration of greenhouse gases is 30% above the benchmark pre-industrial content, rising to ...
“Climate Change” as one of the TOP
“Climate Change” as one of the TOP

... …. There is also a large discrepancy between the immediate time horizon employed by most business and political leaders and the long-term approach required to tackle risks on a global scale…. ...
The “Known” Projections of human drivers
The “Known” Projections of human drivers

... The Unknowns (and why) Forcings: 1. Feedbacks of clouds on climate 2. Temporal and spatial variance in all physical variables 3. Tropical cyclone effects on ventilation (reduction of the “dead zone”) 4. Effects of human behavior on climate change forcing (CO2, land use, etc.) Biodiversity: 1. Relat ...
Results: Impacts to Demand
Results: Impacts to Demand

... • Borehole temperatures indicate warming • But: not every station shows warming; upper-air temperatures not increasing (satellites, balloons) ...
press release
press release

... the  main  cause  of  the  Pacific  wind,   Waves  crashing  over  roadway  in  Temwaiku,  Kiribati.  Courtesy  of   temperature,   and   sea   level   trends   Annika  Dean.   over   the   past   20   years   lies   in   the   Atlantic ...
Climate Change
Climate Change

... •climate millions of years ago: global temperature and CO2 levels higher •climate over the last million years: variations in temperature and CO2 levels •climate over the last few thousand years to present: global temperatures rise at time of industrial revolution ...
Critiquing “The Day After Tomorrow” and “An
Critiquing “The Day After Tomorrow” and “An

6. Integrating Climate Change
6. Integrating Climate Change

... -Developing a climate change plan in 2012 for end-to-end integration of climate change by 2015 -Integrating climate change considerations into all aspect of operations and employees program of work. ...
INTRODUCTION
INTRODUCTION

... that the release of fossil fuels will prevent increasing percentages of outgoing thermal energy from permanently leaving the surface of the earth. (ALLEN 2001) In 2001, the Intergovernmental Panel on Climate Change (IPCC) found that the earth will continue to warm over the course of the next 100 yea ...
Global Temperature Change
Global Temperature Change

... Perry and Hsu (2000) using a solar-luminosity model based solar-related isotopes-variations scanned 90,000-year glacial cycle. They observed excellent correlation using carbon-14 variations and carefully dated tree rings data as far back as the Medieval Warming (900-1300 AD). They extrapolated findi ...
Earth,Notes,RevQs,Ch21
Earth,Notes,RevQs,Ch21

... 14. Based on the increase in global average surface temperature during the twentieth century when carbon dioxide levels were increasing, temperatures in the lower atmosphere are likely to increase in the future as carbon dioxide levels continue to increase. 15. Other trace gases that are contributin ...
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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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