The Rough Guide to Climate ChangeThe Rough Guide to Climate Change gives the complete picture of the single biggest issue facing the planet. Cutting a swathe through scientific research and political debate, this completely updated 2nd edition lays out the facts and assesses the options- global and personal- for dealing with the threat of a warming world. The guide looks at the evolution of our atmosphere over the last 4.5 billion years and what computer simulations of climate change reveal about our past, present, and future. This updated edition includes new information from the 2007 report from the Intergovernmental Panel on Climate Change and an updated politics section to reflect post-Kyoto developments. Discover how rising temperatures and sea levels, plus changes to extreme weather patterns, are already affecting life around the world. The guide unravels how governments, scientists and engineers plan to tackle the problem and includes in-depth information and lifestyle tips about what you can do to help. |
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Page 89
... melting . The changes have been equally dramatic along Greenland's margins . This is apparently due to increased warm - weather runoff as well as an important process called dynamic thinning . When meltwater seeps through a flowing ...
... melting . The changes have been equally dramatic along Greenland's margins . This is apparently due to increased warm - weather runoff as well as an important process called dynamic thinning . When meltwater seeps through a flowing ...
Page 96
... melting , the ice cap would quickly revert to a smoother - edged contour . This suggests the Sun rather than the air is the prime melting agent . More evidence for the Sun's key role is the east - west orientation of Kilimanjaro's ice ...
... melting , the ice cap would quickly revert to a smoother - edged contour . This suggests the Sun rather than the air is the prime melting agent . More evidence for the Sun's key role is the east - west orientation of Kilimanjaro's ice ...
Page 105
... melting . Across eastern Africa , the scanty data show little if any warming trend , which means that drying and other factors may be teaming up to produce Kilimanjaro's rapid ice loss ( see p.96 ) . Aside from temperature , there's a ...
... melting . Across eastern Africa , the scanty data show little if any warming trend , which means that drying and other factors may be teaming up to produce Kilimanjaro's rapid ice loss ( see p.96 ) . Aside from temperature , there's a ...
Contents
The greenhouse effect | 20 |
The symptoms | 43 |
Floods droughts | 58 |
Copyright | |
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2007 IPCC report amount Antarctica Arctic areas assessment atmosphere Australia average carbon dioxide carbon footprint Center century climate change climate models climateprediction.net clouds CO₂ computer models cooling countries crops decades drought Earth efficiency El Niño electricity energy environmental especially Europe factors flooding forests fossil fuels glaciers global climate global models global temperature global warming greenhouse effect greenhouse emissions greenhouse gases Greenland Hadley Centre heat wave hurricanes hydrogen ice age ice sheets impact increase intense IPCC Kyoto Protocol land less Little Ice Age major melting methane million years ago National Niño North America North Atlantic nuclear ocean offset overall ozone permafrost plants produce rain rainfall recent reduce reefs regions Research risk satellite sceptics sea level sea-level rise shift snow solar storms summer sunlight surface there's trees trend tropical cyclones typically warmer water vapour weather wind