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GlobWarm12.Hoboken_s
GlobWarm12.Hoboken_s

Climate Fact Sheet - South Carolina Sea Grant Consortium
Climate Fact Sheet - South Carolina Sea Grant Consortium

30 Oct 2004
30 Oct 2004

... within a few decades; and breakup of the mile-thick West Antarctic Ice Sheet. There are recent reports that this last disaster, the breakup of the WAIS, may be already beginning. Although it would take thousands of years for global warming to directly melt the entire WAIS, there are subtle ways to d ...
Impact of climate change
Impact of climate change

Ch 19 - Miss Clark's Website
Ch 19 - Miss Clark's Website

The implication of rapid Polar warming to the tropics
The implication of rapid Polar warming to the tropics

Carbon Dioxide Emission
Carbon Dioxide Emission

... Some gases in the atmosphere allow visible light to pass through, but they block much of the heat which is reflected from Earth's surface — in the same way as the glass windows in a greenhouse. Without this greenhouse effect, temperatures in the world would be lower by 35 degrees Celsius, most of th ...
1. - Scholastic
1. - Scholastic

... you’ll read about the increase in the number of extreme weather events. Many scientists believe that climate change is contributing to this phenomenon, but they admit that they can’t prove it. What is the difference between weather and climate? Weather refers to specific, short-term events such as a ...
February 2008 - UP Beta Sigma
February 2008 - UP Beta Sigma

... Lately, however, I have strived to become a more discerning iceman because of what has been appearing in the news. Or disappearing, to be more precise. Here’s the skinny. Recent surveys of ice in the arctics show that glaciers are melting faster than predicted by computer modeling. What’s more, the ...
Timmermann's PowerPoint
Timmermann's PowerPoint

... The rate of sea level rise since the mid-19th century has been larger than the mean rate during the previous two millennia (high confidence). Over the period 1901–2010, global mean sea level rose by 0.19 [0.17 to 0.21] m ...
Unit 6 The Warmer the Worse
Unit 6 The Warmer the Worse

Document
Document

... converge toward Equator as shallow surface water to continue warming ...
Climate Change Impacts in the Amazon
Climate Change Impacts in the Amazon

... Some of the infrared radiation passes through the atmosphere, and some is absorbed and re-emitted in all directions by greenhouse gas molecules. The effect of this is to warm the Earth’s surface and the lower atmosphere. ...
Global Warming, the End of Life as We Know It?
Global Warming, the End of Life as We Know It?

... relevant to understanding the scientific basis of risk of humaninduced climate change, its potential impacts and options for adaptation and mitigation” – This agency does NOT carry out research or monitor climate data – The basic assessments made are on peer reviewed and published scientific/ techni ...
Chapter 20 Climate Change and Ozone Depletion Core Case Study
Chapter 20 Climate Change and Ozone Depletion Core Case Study

Notes 19.3
Notes 19.3

... world’s species, longer and more intense heatwaves just to name a few - Temperatures are rising rapidly globally - Harmful effects will be unevenly distributed • Tropics will have more fluctuating temperatures, sea-level rises, and droughts. - Climate change tipping points will occur – thresholds be ...
File
File

Climate Change and Conservation
Climate Change and Conservation

Diapositiva 1
Diapositiva 1

Social Movements
Social Movements

Dr. Ron Sass Department of Ecology and Evolutionary
Dr. Ron Sass Department of Ecology and Evolutionary

Chapter 16 - Global Climate
Chapter 16 - Global Climate

Brian Hoskins Presentation - Climate Change
Brian Hoskins Presentation - Climate Change

... parameters Explosive volcanoes ...
climate change and ozone depletion
climate change and ozone depletion

Effects of Global Warming on Weather and Climate
Effects of Global Warming on Weather and Climate

< 1 ... 93 94 95 96 97 98 99 100 101 ... 105 >

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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