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... petroleum) are burned. Use of fossil fuels is an essential part of our everyday lives, primarily through transport, heating and other energy consumption. In this way, we are all responsible, on an individual and national level. THEORY: As with many scientific theories, global warming is not yet conc ...
presentation - The Greater Thames Marshes Nature Improvement Area
presentation - The Greater Thames Marshes Nature Improvement Area

... – Covers all identified impacts of climate change – Including indirect impacts (although there are areas where we need wider consultation with external organisations) – Identifies gaps in our knowledge – Informs future projects ...
doc
doc

... 1. How has solar variability contributed to large-scale (continental,hemispheric, global) climate variations during the Holocene? 2. Why was the Sahara wet during a portion of the Holocene? 3. How do dissociation of clathrates contribute to abrupt warming events? 4. How does the frequency and intens ...
Env_Prior_Net - Department of Atmospheric and Oceanic Sciences
Env_Prior_Net - Department of Atmospheric and Oceanic Sciences

... also implies an increase in precipitation, because the atmosphere can’t store water vapor indefinitely. There is no clear consensus on how the increase in precipitation will be distributed. However, we do know that it will not be distributed uniformly. This increase in evaporation and precipitation ...
Salinger, Dr Jim (10.9 MB PowerPoint)
Salinger, Dr Jim (10.9 MB PowerPoint)

... Ocean acidification ...
Global Warming - Florida International University
Global Warming - Florida International University

... • Sea surface-temperature is one important type of data that GOES and POES provide. • Temperature changes influence the behavior of fish, can cause the bleaching of corals, and affects weather along the coast. • Satellite images of sea-surface temperature also show patterns of water circulation. Exa ...
The Forest Service Climate Change Performance Scorecard
The Forest Service Climate Change Performance Scorecard

... The Forest Service Climate Change Performance Scorecard Each national forest and grassland is expected to do seven of the following by 2015: ...
Intro to climate system
Intro to climate system

... The trend is part of a natural cycle The trend is part of anthropogenic climate change The trend is caused by volcanic activity and solar cycles ...
Climate Trends Along the St. John River, Presesentation for “Water
Climate Trends Along the St. John River, Presesentation for “Water

... • Provincial leadership on climate change. • Reduce or prevent GHG emissions. • Adaptation strategies to address economic, social & environmental impacts. • Collaboration at provincial, regional, national, and international levels. • Engagement and mainstreaming. ...
japan
japan

... In Japan, relatively low temperatures continued up until the 1940s, but then started to rise. After experiencing high temperatures in around the 1960s and rather low temperatures until the mid-1980s, the temperature rapidly rose from the late 1980s. Many of the years that marked record-high temperat ...
i3084e25
i3084e25

... In Japan, relatively low temperatures continued up until the 1940s, but then started to rise. After experiencing high temperatures in around the 1960s and rather low temperatures until the mid-1980s, the temperature rapidly rose from the late 1980s. Many of the years that marked record-high temperat ...
Under 2 Degrees Celsius: - Veerabhadran Ramanathan
Under 2 Degrees Celsius: - Veerabhadran Ramanathan

... “It is still not too late to limit the warming. Staying below 2ºC requires social, financial, and technical actions by 2020 on a global scale. Transitioning to the energy of the future and cleaning the air of short lived pollutants are critical steps to the health and well being of the most vulnerab ...
Climate Change and the Marine Environment
Climate Change and the Marine Environment

... •Over Fishing •Oil Spills ...
Foreword by R.K. Pachauri, Chair of the IPCC
Foreword by R.K. Pachauri, Chair of the IPCC

Global Warming is Hot Stuff!
Global Warming is Hot Stuff!

... what they are today if we don’t reduce the burning of fossil fuels! ...
ClimateChange1
ClimateChange1

... It is likely that this warming is larger than for any century since 200AD, and that the 1990s were the warmest decade in the last millennium. The warming differs in different parts of the world, but over the last 25 years, almost everywhere has warmed, and very few places have cooled. Other changes ...
II. Changes in climate
II. Changes in climate

... Easterling, W.E., et al. 2007: Food, fibre and forest products. Climate Change 2007: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, M.L. Parry, O.F. Canziani, J.P. Palutikof, P.J. van der Linde ...
Climate Change in New York Recent Trends and Future
Climate Change in New York Recent Trends and Future

... • Annual temperatures across New York have warmed almost 2º F since 1970 • Winter temperatures have warmed by nearly 5! F since 1970 • More extremes in rainfall • Most places are less snowy except LES • The growing season as enlongated ...
Evolution of the climate science
Evolution of the climate science

... “Warming of the climate system is unequivocal” “Over 90% probability that this global warming is primarily caused by human activities – the most important of these being the emission of greenhouse gases and the clearing of natural vegetation”. - IPCC Fourth Assessment Report ...
Economics of Ecosystems and Biodiversity in Jordan
Economics of Ecosystems and Biodiversity in Jordan

... decrease in precipitation in the majority of meteorological stations. Only 2 out of 19 stations show an increase of 5-10% in precipitation at the same time. ...
Dear Gary Johnson
Dear Gary Johnson

... a. Authors, who donate their time, are selected on the basis of their expertise in consultation with all member countries and include experts in the fields of meteorology, physics, oceanography, statistics, engineering, ecology, social sciences and economics. b. After completion of the draft documen ...
Debate on Climate Shifts to Issue of Irreparable Change
Debate on Climate Shifts to Issue of Irreparable Change

... States and abroad, because the answer could determine how drastically countries need to reduce their greenhouse gas emissions in the coming years. While scientists remain uncertain when such a point might occur, many say it is urgent that policymakers cut global carbon dioxide emissions in half over ...
Climate change vulnerability and adaptation research at TERI
Climate change vulnerability and adaptation research at TERI

... In a case study of the Lakhwar watershed in northern India, it was found that about 1500 km2 of the total 4000 km2 of the watershed receives an annual runoff of less than 1250 mm, and is highly sensitive to increased water stress due to climate change. To asses the relative vulnerability of India's ...
Knowledge for development under climate change Habiba Gitay
Knowledge for development under climate change Habiba Gitay

... –Improved energy efficiency and conservation –cleaner oil and coal technologies; –renewable energy, including solar, wind and hydropower; –market mechanisms for carbon trading –the role of forestry and agriculture, including reduced emissions from deforestation and degradation (REDD), –policy instru ...
FACT SHEET #4: Historic and Projected Climate Change
FACT SHEET #4: Historic and Projected Climate Change

... current atmospheric CO2 levels have risen approximately 138 percent above those of the pre-industrial period (Tans, 2010). ...
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Effects of global warming



The effects of global warming are the environmental and social changes caused (directly or indirectly) by human emissions of greenhouse gases. There is a scientific consensus that climate change is occurring, and that human activities are the primary driver. Many impacts of climate change have already been observed, including glacier retreat, changes in the timing of seasonal events (e.g., earlier flowering of plants), and changes in agricultural productivity.Future effects of climate change will vary depending on climate change policies and social development. The two main policies to address climate change are reducing human greenhouse gas emissions (climate change mitigation) and adapting to the impacts of climate change. Geoengineering is another policy option.Near-term climate change policies could significantly affect long-term climate change impacts. Stringent mitigation policies might be able to limit global warming (in 2100) to around 2 °C or below, relative to pre-industrial levels. Without mitigation, increased energy demand and extensive use of fossil fuels might lead to global warming of around 4 °C. Higher magnitudes of global warming would be more difficult to adapt to, and would increase the risk of negative impacts.
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