Unstoppable Global Warming: Every 1,500 YearsSupported by in-depth scientific evidence, Singer and Avery present the compelling concept that global temperatures have been rising mostly or entirely because of a natural cycle. Unstoppable Global Warming explains why we're warming, why it's not very dangerous, and why we can't stop it anyway. |
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... higher Earth latitudes. There is only one large continental landmass, Gondwana, in the southern hemisphere. 300 million years ago: Earth uniformly hot and humid, land area dominated by swamps and rain forest. 250 million years ago ...
... higher Earth latitudes. There is only one large continental landmass, Gondwana, in the southern hemisphere. 300 million years ago: Earth uniformly hot and humid, land area dominated by swamps and rain forest. 250 million years ago ...
Page xiii
... higher Earth latitudes . There is only one large continental landmass , Gondwana , in the southern hemisphere . 300 million years ago : Earth uniformly hot and humid , land area dominated by swamps and rain forest . 250 million years ...
... higher Earth latitudes . There is only one large continental landmass , Gondwana , in the southern hemisphere . 300 million years ago : Earth uniformly hot and humid , land area dominated by swamps and rain forest . 250 million years ...
Page xiv
... higher latitudes.1 THE MORE RECENT CLIMATE TIMELINE 130,000 to 110,000 years ago: Eemian interglacial, warm. 110,000 years ago: Fairly sudden shift to much-colder-than-present glacial conditions, over perhaps four hundred years—or even ...
... higher latitudes.1 THE MORE RECENT CLIMATE TIMELINE 130,000 to 110,000 years ago: Eemian interglacial, warm. 110,000 years ago: Fairly sudden shift to much-colder-than-present glacial conditions, over perhaps four hundred years—or even ...
Page 17
... higher tempera- tures could overwhelm the Great Atlantic Conveyor, the huge ocean current that distributes heat from the equator to the poles. The Gulf Stream would then shut down, and we would all be covered in ice before you can say ...
... higher tempera- tures could overwhelm the Great Atlantic Conveyor, the huge ocean current that distributes heat from the equator to the poles. The Gulf Stream would then shut down, and we would all be covered in ice before you can say ...
Page 36
... higher CO , concentrations . It is hard to know how fast the Earth's highly variable sur- face is warming , but it is warming faster than the lower atmosphere where the CO2 is accumulating . This is strong evidence that CO2 is not the ...
... higher CO , concentrations . It is hard to know how fast the Earth's highly variable sur- face is warming , but it is warming faster than the lower atmosphere where the CO2 is accumulating . This is strong evidence that CO2 is not the ...
Contents
1 | |
21 | |
35 | |
45 | |
The Treaty that Would Change Earths Climate | 55 |
The Baseless Fears A Million Wild Species Will Be Lost Forever | 75 |
Warming and Cooling in Human History | 97 |
The Baseless Fears Warming Brings Famine | 117 |
How Far Can We Trust the Global Climate Models? | 175 |
The Baseless Fears Abrupt Global Cooling | 187 |
The SunClimate Connection | 191 |
The Baseless Fears Millions of Human Deaths from Warming | 201 |
Powering the Future | 209 |
The Ultimate Failure of the Kyoto Protocol | 221 |
Glossary | 235 |
Index | 247 |
The Earth Tells Its Own Story of Past Climate Cycles | 127 |
The Baseless Fears More Frequent and Fiercer Storms | 161 |
About the Authors | 259 |
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Unstoppable Global Warming: Every 1,500 Years, Part 1 Siegfried Fred Singer,Dennis T. Avery Limited preview - 2007 |
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