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xi | |
Foreword |
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xv | |
Preface |
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xvii | |
Acknowledgments |
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xix | |
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1 | (12) |
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Why a hundred thousand years? |
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1 | (4) |
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5 | (2) |
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Management and cooperation |
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7 | (2) |
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The overall plan of the book |
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9 | (2) |
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11 | (2) |
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A Brief History of the Earth |
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13 | (40) |
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13 | (3) |
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16 | (2) |
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The formation of the Moon and the Late Heavy Bombardment |
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18 | (5) |
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Continents and plate tectonics |
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23 | (8) |
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23 | (1) |
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24 | (4) |
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The Earth's magnetic field |
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28 | (3) |
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Evolution of the Earth's atmosphere |
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31 | (4) |
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35 | (13) |
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The early fossils in the Archean |
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35 | (2) |
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The Proterozoic and the apparition of oxygen |
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37 | (1) |
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The Neo-Proterozoic: the Ediacarans and the `snowball earth' |
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38 | (5) |
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The Phanerozoic, life extinctions |
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43 | (5) |
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48 | (1) |
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48 | (5) |
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53 | (40) |
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53 | (1) |
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54 | (8) |
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57 | (1) |
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Encounters with interstellar clouds and stars |
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57 | (2) |
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Supernovae explosions, UV radiation and cosmic rays |
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59 | (1) |
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Gamma-ray bursts and magnetars |
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60 | (2) |
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62 | (27) |
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62 | (4) |
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The nature of the impactors: asteroids and comets |
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66 | (7) |
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73 | (3) |
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The bombardment continues |
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76 | (4) |
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80 | (1) |
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Deviation from the dangerous path |
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80 | (4) |
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84 | (1) |
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85 | (4) |
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89 | (1) |
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89 | (4) |
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93 | (60) |
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93 | (2) |
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95 | (7) |
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How old shall we be in 1,000 centuries? |
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98 | (2) |
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How tall shall we be in 1,000 centuries? |
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100 | (2) |
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Seismic hazards: the threat of volcanoes |
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102 | (13) |
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Volcanoes and tectonic activity |
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102 | (4) |
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The destructive power of volcanoes |
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106 | (3) |
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Volcanoes and climate change |
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109 | (3) |
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112 | (3) |
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Seismic hazards: the threat of earthquakes |
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115 | (10) |
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Measuring the power of earthquakes |
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119 | (1) |
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120 | (5) |
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Mitigation against earthquakes |
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125 | (1) |
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125 | (7) |
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125 | (2) |
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The 26 December 2004 Sumatra tsunami |
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127 | (1) |
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Forecasting tsunamis and mitigation approaches |
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128 | (4) |
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132 | (14) |
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Storms: cyclones, hurricanes, typhoons, etc. |
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132 | (5) |
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137 | (5) |
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142 | (4) |
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146 | (2) |
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148 | (5) |
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153 | (34) |
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Miscellaneous evidence of climate change |
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153 | (3) |
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The global climate system |
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156 | (4) |
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Climates in the distant past |
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160 | (3) |
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163 | (8) |
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171 | (3) |
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174 | (2) |
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176 | (1) |
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177 | (1) |
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Interpretation of the recent record |
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178 | (1) |
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179 | (3) |
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182 | (5) |
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187 | (26) |
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Scenarios for future climates |
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188 | (6) |
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Geographic distribution of warming |
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194 | (3) |
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197 | (4) |
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The 100,000-year climate future |
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201 | (4) |
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205 | (1) |
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Consequences of climate change |
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206 | (1) |
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207 | (2) |
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The four main SRES scenarios |
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207 | (2) |
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209 | (4) |
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The Future of Survivability: Energy and Inorganic Resources |
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213 | (40) |
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213 | (19) |
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Energy requirements for the 100,000-year world |
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215 | (2) |
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Minor energy sources for the long-term future |
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217 | (2) |
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219 | (2) |
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221 | (2) |
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223 | (2) |
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225 | (3) |
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228 | (4) |
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Energy for the present century |
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232 | (6) |
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232 | (4) |
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Electricity and renewables |
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236 | (1) |
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236 | (2) |
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238 | (12) |
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Abundances and formation of the elements |
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238 | (3) |
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The composition of the Earth |
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241 | (1) |
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242 | (2) |
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244 | (1) |
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Mineral resources for 100,000 years |
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245 | (5) |
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250 | (1) |
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250 | (1) |
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250 | (3) |
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The Future of Survivability: Water and Organic Resources |
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253 | (28) |
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253 | (10) |
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254 | (1) |
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Water use and water stress |
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255 | (2) |
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257 | (3) |
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260 | (2) |
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From now to then: water and climate change |
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262 | (1) |
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263 | (8) |
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263 | (2) |
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Present and past land use |
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265 | (1) |
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266 | (1) |
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Agricultural land and production |
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266 | (1) |
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267 | (1) |
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Fertilizers and pesticides |
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267 | (1) |
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267 | (2) |
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Agriculture for 100,000 years |
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269 | (2) |
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271 | (1) |
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271 | (5) |
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273 | (3) |
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276 | (1) |
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276 | (5) |
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Leaving Earth: From Dreams to Reality? |
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281 | (34) |
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281 | (1) |
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282 | (18) |
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284 | (4) |
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288 | (6) |
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294 | (3) |
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297 | (2) |
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299 | (1) |
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What to do with the Moon? |
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300 | (8) |
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301 | (2) |
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The Moon as a scientific base |
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303 | (1) |
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The Moon for non-scientific exploitation |
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303 | (3) |
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Resources from outside the Earth-Moon system: planets and asteroids |
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306 | (2) |
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308 | (3) |
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308 | (1) |
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309 | (2) |
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311 | (1) |
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311 | (4) |
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Managing the Planet's Future: The Crucial Role of Space |
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315 | (52) |
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315 | (1) |
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The specific needs for space observations of the Earth |
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316 | (13) |
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316 | (3) |
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Water: the hydrosphere and the cryosphere |
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319 | (4) |
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323 | (4) |
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327 | (2) |
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The tools and methods of space |
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329 | (33) |
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The best orbits for Earth observation |
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330 | (1) |
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Geodesy and altimetry satellites: measuring the shapes of the Earth |
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331 | (6) |
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Global Positioning Systems |
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337 | (2) |
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Synthetic Aperture Radars |
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339 | (8) |
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347 | (3) |
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Remote-sensing spectroscopy |
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350 | (4) |
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354 | (3) |
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Monitoring astronomical and solar influences |
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357 | (5) |
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362 | (1) |
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363 | (4) |
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Managing the Planet's Future: Setting-Up the Structures |
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367 | (36) |
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367 | (1) |
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The alert phase: need for a systematic scientific approach |
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368 | (13) |
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Forecasting the weather: the `easy' case |
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368 | (4) |
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The scientific alert phase: the example of the IPCC |
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372 | (4) |
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Organizing the space tools |
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376 | (5) |
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The indispensable political involvement |
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381 | (16) |
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The crucial role of the United States, China and India |
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381 | (3) |
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A perspective view on the political perception |
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384 | (9) |
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The emotional perception: the scene is moving |
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393 | (4) |
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Conclusion: towards world ecological governance? |
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397 | (2) |
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399 | (4) |
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403 | (12) |
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Limiting population growth |
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403 | (2) |
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Stabilizing global warming |
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405 | (1) |
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The limits of vessel-Earth |
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406 | (1) |
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The crucial role of education and science |
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407 | (1) |
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408 | (2) |
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The difficult and urgent transition phase |
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410 | (1) |
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Adapting to a static society |
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411 | (2) |
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413 | (2) |
Index |
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415 | |