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Helping SE Communities Think about Climate Change and Adaptation
Helping SE Communities Think about Climate Change and Adaptation

Notes
Notes

... past may become a permanent fixture. • Similar effects may be felt in other recreational areas, including ice fishing, snowmobiling, skiing, and other winter- or water-based sports. Source: www.ducks.org ...
Week Nine
Week Nine

...  University of Arizona Sea Level Animation ...
PowerPoint - Columbia University
PowerPoint - Columbia University

Project Description
Project Description

222
222

... The global green house gas emissions due to anthropogenic activities have increased since preindustrial times with increase of about 70% between 1970 and 2004 (IPCC 2007). The major effect of the increase of anthropogenic green house gas emissions in the atmosphere is global warming. It has been est ...


melting -actic - Classroom Encounters
melting -actic - Classroom Encounters

NRDC: Miami and the Keys, Florida: Identifying and Becoming More
NRDC: Miami and the Keys, Florida: Identifying and Becoming More

Nine Lies About Global Warming
Nine Lies About Global Warming

2011 Annual Report
2011 Annual Report

... HMMV, where they used on-board sonar to image methane bubbles coming up through the water column; employed a new sub-bottom profiler—some six years in the making—to map the mud structures; and deployed TETHYS to conduct in situ measurements of HMMV emissions in order to determine if they were carbon ...
PDF sample
PDF sample

Workshop-2-Impacts-FINAL
Workshop-2-Impacts-FINAL

PDF: Printable Version
PDF: Printable Version

Major Ocean Currents
Major Ocean Currents

A. Global Warming Project - University of Wisconsin
A. Global Warming Project - University of Wisconsin

Fish and climate
Fish and climate

... http://joannenova.com.au/2009/12/newscientist-becomes-non-scientist/ ...
Present - Princeton University
Present - Princeton University

The Ganges-Brahmaputra Delta in a Changing Climate
The Ganges-Brahmaputra Delta in a Changing Climate

citizen science - City of Del Mar
citizen science - City of Del Mar

Day 2, Resources
Day 2, Resources

... • historical data about how weather and climate changes have affected people; • climate data and predictions to determine how best to serve the needs of people now and prepare for future climate change. Information about a Warming Climate • The United State produces more greenhouse gases than any ...
CLIMATE WARS Programme 1: The science Two Harvard
CLIMATE WARS Programme 1: The science Two Harvard

Global warming - University of Dayton
Global warming - University of Dayton

A glacier is a slow-moving, extended mass of ice
A glacier is a slow-moving, extended mass of ice

Model-simulated CO2-induced changes in seasonal precipitation
Model-simulated CO2-induced changes in seasonal precipitation

< 1 ... 63 64 65 66 67 68 69 70 71 ... 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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