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chapter 19
chapter 19

... agricultural soils or retiring agricultural land and allowing it to become pasture or forest. Researchers are looking at cost-effective ways of capturing CO2 from the air, from coal-burning power stations, and from other emission sources. This captured CO2 would be compressed and pumped into abandon ...
Ch 19 - Yourclasspage.com
Ch 19 - Yourclasspage.com

... agricultural soils or retiring agricultural land and allowing it to become pasture or forest. Researchers are looking at cost-effective ways of capturing CO2 from the air, from coal-burning power stations, and from other emission sources. This captured CO2 would be compressed and pumped into abandon ...
Chapter 2: The Physical Setting
Chapter 2: The Physical Setting

Global Warming Notes
Global Warming Notes

How much climate change can we bear?
How much climate change can we bear?

... Estimates of the ‘sensitivity’ of the climate to increases in ghgs are expressed in terms of the temperature response of the climate system to a doubling of preindustrial levels of greenhouse gases in the atmosphere, expressed in carbondioxide equivalence in parts-per-million (ppm). Pre-industrial l ...
Atmosphere and Change 2
Atmosphere and Change 2

... Even though the number of humans in some of the eras and ages shown in those charts was far smaller than what it is now, Greenland was never a much populated place ...
Global Warming and Climate Change in a Nutshell
Global Warming and Climate Change in a Nutshell

... global temperature increase of 4° C (7.2° F) is about the difference between temperatures today and those in the last ice age when much of central Europe and North America were covered with kilometers of ice. Claims of Global Warming Pause: Some climate skeptics claim that there has been no global ...
The chaos created by the Climate Liars of Copenhagen who say
The chaos created by the Climate Liars of Copenhagen who say

... warmth over hundreds of thousands of years - extremes far in excess of modern temperature changes. 3. The 2009 minimum Arctic ice extent was significantly larger than the previous two years. The 2009 Antarctic maximum ice extent was significantly above the 30-year average. There are only 30 years of ...
Lecture 03
Lecture 03

... a world in which the emphasis is on local solutions to economic, social and environmental sustainability. It is a world with continuously increasing global population, at a rate lower than A2, intermediate levels of economic development, and less rapid and more diverse technological change than in t ...
Lecture 02
Lecture 02

... a world in which the emphasis is on local solutions to economic, social and environmental sustainability. It is a world with continuously increasing global population, at a rate lower than A2, intermediate levels of economic development, and less rapid and more diverse technological change than in t ...
File - Down the Rabbit Hole
File - Down the Rabbit Hole

... shows 5% stepwise drop during 1980s ...
The current causes of climate change: the human causes
The current causes of climate change: the human causes

Global Warming, Advocacy Global warming refers to an unequivocal
Global Warming, Advocacy Global warming refers to an unequivocal

Salinger, Dr Jim (10.9 MB PowerPoint)
Salinger, Dr Jim (10.9 MB PowerPoint)

Top Ten Things You Need to Know about Global Warming
Top Ten Things You Need to Know about Global Warming

Presentation Slides From IPCC
Presentation Slides From IPCC

Slide 1
Slide 1

Climate change and the probability of extreme events
Climate change and the probability of extreme events

... Rainfall intensity Precipitation in extratropics Hurricane intensity Drought Extreme high temperatures Heat waves ...
class viii science theme 2
class viii science theme 2

... As John Cook, creator of the graphic above says (see above link), Just as it takes time for a cup of coffee to release heat into the air, so to it takes time for the ocean to release its heat into the atmosphere.. Indeed, as this chart also shows, the warming in the oceans has been occurring for qui ...
Hazards
Hazards

Duka_Castillo_The effects of climate change on New York City
Duka_Castillo_The effects of climate change on New York City

The Future
The Future

Pacific Ocean waters absorbing heat 15 times faster over past 60
Pacific Ocean waters absorbing heat 15 times faster over past 60

U3A-ClimChange06 10384KB Oct 27 2012
U3A-ClimChange06 10384KB Oct 27 2012

... end of the Younger Dryas cold period we discussed last week • The Holocene epoch has been a period of climatic stability compared with the Last Glacial that preceded it • Nevertheless, even minor changes have had major impacts on human activities, both in prehistoric and historic times ...
Past Climates
Past Climates

... Nine current tipping elements vulnerable to possible abrupt change. The time frames and threshold temperature increases may be modified with more data. Region Indian Summer Monsoon ...
< 1 ... 97 98 99 100 101 102 103 104 >

Future sea level



The rate of global mean sea-level rise (~3 mm/yr; SLR) has accelerated compared to the mean of the 20th century (~2 mm/yr), but the rate of rise is locally variable. Factors contributing to SLR include decreased global ice volume and warming of the ocean. On Greenland, the deficiency between annual ice gained and lost tripled between 1996 and 2007. On Antarctica the deficiency increased by 75%. Mountain glaciers are retreating and the cumulative mean thickness change has accelerated from about −1.8 to −4 m in 1965 to 1970 to about −12 to −14 m in the first decade of the 21st century. From 1961 to 2003, ocean temperatures to a depth of 700 m increased and portions of the deeper ocean are warming.The Intergovernmental Panel on Climate Change (2007) projected sea level would reach 0.18 to 0.59 m above present by the end of the 21st century but lacked an estimate of ice flow dynamics calving. Calving was added by Pfeffer et al. (2008) indicating 0.8 to 2 m of SLR by 2100 (favouring the low end of this range). Rahmstorf (2007) estimated SLR will reach 0.5 to 1.4 m by the end of the century. Pielke (2008) points out that observed SLR has exceeded the best case projections thus far. These approximations and others indicate that global mean SLR may reach 1 m by the end of this century. However, sea level is highly variable and planners considering local impacts must take this variability into account.
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