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Meeting the Climate-Change Challenge John P. Holdren
Meeting the Climate-Change Challenge John P. Holdren

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Coastal cities inundated, farming regions parched, ocean currents

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... North Atlantic Ocean and the Canadian Arctic ArcTrain is a collaborative project between the University of Bremen and the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research in Germany, and a consortium of eight Canadian universities led by the Université du Québec à Montréal. F ...
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... FIGURE 19-16 Future changes in subsurface ocean temperature Measuring increases in the height of the ocean caused by thermal expansion and increases in the velocity of sound moving through subsurface ocean layers (A SOund Fixing And Ranging Channel located at a depth near 1 km is particularly ...
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... compiled by Germanwatch, an international nongovernmental organization that works on environment and development issues [9]. The effects of global warming leads to climate change in various aspects. Though all the climate change aspects are related to each other, they are described below separately. ...
A Changing Climate: Cold adventures
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... and Mawson only escaped death after falling into a crevasse because his sledge became jammed in the ice, leaving him dangling from a rope. It was a terrible ordeal. The explorers were so exhausted and hungry that they had to eat their dogs to survive. One man, Belgrave Ninnis, fell down a snow-cover ...
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Grantham Briefing Note 4 – September 2013 The Earth`s energy

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October 4, 2009 Arctic Ocean acid `will dissolve

... Opting Out of Migration: As Climate Warms, Arctic-Nesting Geese Elect to Winter in Alaska Instead of Mexico U.S. Department of Interior Press Release Until recently, nearly the entire (90 percent) population of Pacific brant wintered in Mexico, but now as many as to 30 percent are opting to spend th ...
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climatechange - Otterville R

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... CO2 over the last 160,000 yr  Current concentrations are higher than any time in at least the past ~780,000 years ...
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Then Now Natural climate variability and change The enhanced

... lower albedo. This exposed surface absorbs more energy from the Sun which, in turn, warms the atmosphere even further. This is like the difference between wearing a black jacket and a white jacket on a sunny day. We feel warmer in a ...
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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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