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PowerPoint Presentation - Community Earth System Model
PowerPoint Presentation - Community Earth System Model

... 5. 1% CO2 run to year 80 where CO2 doubles at year 70 with corresponding control run 6. 100 year (minimum) control run including same time period as in 1 above 7. 2XCO2 equilibrium with atmosphere-slab ocean 8. Extend one A1B and B1 simulation to 2300 9. 1% CO2 run to quadrupling with an additional ...
Assessing the Risk of Climate Change on the Water Resources of
Assessing the Risk of Climate Change on the Water Resources of

... OzClim. These were scaled by estimates of global warming that take into account different rates of greenhouse gas emissions and climate model sensitivity for 2030 and 2070. Daily records of P and Ep within IQQM were then modified according to these scenarios, providing a record of climate variabilit ...
Wilderness, Water, and Climate Change
Wilderness, Water, and Climate Change

... Climate Change Overall temperatures in the Rockies — and around the world — are rising dramatically. The Intergovernmental Panel on Climate Change reports that global mean surface temperature increased by 0.6 degrees Celsius (about 1 degree Fahrenheit) over the 20th century. In the Western Hemisphe ...
Incorporating snow albedo feedback into downscaled temperature
Incorporating snow albedo feedback into downscaled temperature

... and total area covered by snow (third column) for various months at 2081–2100, compared with 1981– 2000, for the business-as-usual greenhouse gas scenario. Red lines represent the average warming for all global climate models downscaled. The warming “bulges” in the temperature column show where snow ...
The main consequence of land degradation is the loss of soil
The main consequence of land degradation is the loss of soil

... The region contains 40 per cent of the plant and animal species of the planet. The biota of all countries is threatened. Only Brazil has 103 bird species threatened. Peru and Colombia occupy the fifth place in the world with 64 species each. A third of Chilean vertebrates are threatened. Brazil also ...
The GCOS Assessment Cycle - Group on Earth Observations
The GCOS Assessment Cycle - Group on Earth Observations

... GEOSS support for IPCC assessments - The GCOS Assessment Cycle 1 -4 February 2011, WMO, Geneva, Switzerland Dr Carolin Richter, Director, Global Climate Observing System Secretariat ...
Evidence for climate change - University at Albany Atmospheric
Evidence for climate change - University at Albany Atmospheric

... (confidence range [0.65-1.06K], units are kelvin)* • Virtually certain that the troposphere has warmed since mid-20th century, but highest confidence is limited to the well observed extratropical Northern Hemisphere • Precipitation over Northern Hemisphere mid-latitudes has increased: • since 1951wi ...
Abrupt Climate Change - Ohio State University
Abrupt Climate Change - Ohio State University

... – There are numerous tipping elements (WAIS, GIS, THC, ENSO, etc.) that have various (and dire) impacts on climate › Varying time scales and “abruptness” › Some well within IPCC projected warming for this century ...
PowerPoint - Princeton University
PowerPoint - Princeton University

... Present-day radiative forcing due to aerosols over the eastern US is comparable in magnitude, but opposite in sign, to global forcing due to CO2. Due to short lifetime, forcing due to aerosols is not uniform across globe. Over the US, radiative forcing due to sulfate aerosols is -2 Wm-2. ...
hamlet_city_of_portland_nov_2007
hamlet_city_of_portland_nov_2007

... Mixed Rain and Snow Basins Along the Coast: Strong increases due to warming and increased precipitation variability (both effects increase flood risk) Inland Snowmelt Dominant Basins: Relatively small overall changes because effects of warming (decreased risks) and increased precipitation variabilit ...
full text pdf
full text pdf

... Energy supply, industry/manufacturing and forestry sectors collectively account for over 60% of all greenhouse gas (GHG) emissions. The forestry’s contribution is basically through deforestation worldwide, as trees cut down to clear space for agriculture and other land uses can no longer absorb carb ...
Disappearing evidence
Disappearing evidence

... information with which to distinguish between natural and anthropogenic causes of the observed warming. Paleoarchives can provide such information by extending the climate record over decadal to millennial time scales. Furthermore, paleodata can be used to predict future ecosystem changes associated ...
Pacific puzzle
Pacific puzzle

... online tool (http://go.nature.com/8VQXYx) that can be used to calculate the rate of warming using various start dates and any of the available data sets. But he warns that there is little to be gained from looking at short-term trends; instead we should be focused on long-term warming. “Drawing simp ...
How much more global warming and sea level rise?
How much more global warming and sea level rise?

... downs in meridional overturning in the respective models (greater percentage-wise in CCSM3 than PCM) are not characterized by less warming over northern Europe in either model. The warming from increases of GHGs overwhelms any tendency for decreased high latitude warming from less northward heat tra ...
Hidalgo, HG, Dettinger, MD, and Cayan, DR, in review, Downscaling
Hidalgo, HG, Dettinger, MD, and Cayan, DR, in review, Downscaling

... Warming already has driven Observed: Less spring snowpack TRENDS (1950-97) in hydroclimatic trends. April 1 snow-water content at Observed: Less snow/more rain ...
Global Warming and Climate Change
Global Warming and Climate Change

... greenhouse gas, and is in fact currently responsible for keeping the earth’s surface temperature nearly 30 degrees Centigrade warmer than it would be if there were none. If, for any reason, warming stops for 20 years (it has already stopped for 11), the ‘‘feedback’’ effect between carbon dioxide and ...
Coupled Ocean and Atmosphere Climate Dynamics
Coupled Ocean and Atmosphere Climate Dynamics

... ENVI3410: Coupled Ocean & Atmsophere Climate Dynamics ...
GEOG 208 Human Dimensions of Global Climate Change
GEOG 208 Human Dimensions of Global Climate Change

... overview  of  the  history  of  climate  change  as  an  environmental  issue,  its  theoretical  discovery,   recent  climate  trends  and  climate  change  scenarios  for  the  21st  century  and  beyond.  The   content  of  this  cours ...
Beat the Uncertainty
Beat the Uncertainty

... Underestimate the impact of climate change to agriculture production, fisheries, and food security. Did not know that CC could bring opportunity for people through strategies such as Green Growth. Top priorities for next 5 years include “increase capacity and understanding” of climate change adaptat ...
Integration of Climate Change Into Watershed Management
Integration of Climate Change Into Watershed Management

... processes. Given the size of this region’s population and industrial base, our actions will also be crucial to Canada’s success in achieving its greenhouse gas reduction targets under the Kyoto Protocol. ...
Climate Change Games Resources Sheet
Climate Change Games Resources Sheet

... BBC’s Climate Challenge – The future is in your hands! You are president of the European Nations and must tackle global climate change from 2000 to 2100. You choose Europe’s policies and try to persuade competing regional blocs to reduce their emissions. http://www.willyoujoinus.com/energyville/ Ene ...
Global Warming Games
Global Warming Games

... BBC’s Climate Challenge – The future is in your hands! You are president of the European Nations and must tackle global climate change from 2000 to 2100. You choose Europe’s policies and try to persuade competing regional blocs to reduce their emissions. http://www.willyoujoinus.com/energyville/ Ene ...
Climate Change and the Economic Recession: Should
Climate Change and the Economic Recession: Should

... long wave radiation. However, this energy becomes trapped within the Earth’s atmosphere by the carbon dioxide contained in it. This natural process has been occurring for thousands of years with carbon dioxide levels changing in the atmosphere; this process creating both the Ice Age and the Earth’s ...
DOCX - World bank documents
DOCX - World bank documents

... stresses arising from climate change further add to the problems that exist today. There are serious concerns about meeting future projected water uses, particularly in the dry season.1 Hydrological changes and sea-level rise will affect the availability of fresh water (saline intrusion) or even phy ...
PPT - Atmospheric Chemistry Modeling Group
PPT - Atmospheric Chemistry Modeling Group

... • Past model studies of the effects of climate change on AQ have focused on partial-derivative perturbations to meteorological variables, e.g., [O3 ]/ T • But the perturbations to different meteorological variables are inherently correlated, and the most important perturbation for AQ is likely to ...
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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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