Climate Change 1995: The Science of Climate Change: Contribution of Working Group I to the Second Assessment Report of the Intergovernmental Panel on Climate ChangeCambridge University Press, 1996 M06 6 - 572 pages The IPCC reports represent the primary source of scientific and technical advice for the implementation of the UN Framework Convention on Climate Change. This assessment therefore forms the standard scientific reference for all those concerned with climate change and its consequences, including policy makers in governments and industry worldwide, and researchers and senior-level students in environmental science, meteorology, climatology, biology, ecology and atmospheric chemistry. |
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Page 6
... north Atlantic thermohaline . circulation and a widespread reduction in diurnal range of temperature . These features too can be explained in terms of identifiable physical mechanisms . The direct and indirect effects of anthropogenic ...
... north Atlantic thermohaline . circulation and a widespread reduction in diurnal range of temperature . These features too can be explained in terms of identifiable physical mechanisms . The direct and indirect effects of anthropogenic ...
Page 27
... North Atlantic Ocean north of 30 ° N , and some surrounding land areas , have cooled in recent decades ( Figure 9 ) . As predicted in IPCC ( 1992 ) and discussed in IPCC ( 1994 ) , relatively cooler global surface and tropospheric ...
... North Atlantic Ocean north of 30 ° N , and some surrounding land areas , have cooled in recent decades ( Figure 9 ) . As predicted in IPCC ( 1992 ) and discussed in IPCC ( 1994 ) , relatively cooler global surface and tropospheric ...
Page 28
... North Atlantic , and were probably linked to changes in oceanic circulation . These rapid changes suggest that climate may be quite sensitive to internal or external climate forcings and feedbacks . The possible relevance of these rapid ...
... North Atlantic , and were probably linked to changes in oceanic circulation . These rapid changes suggest that climate may be quite sensitive to internal or external climate forcings and feedbacks . The possible relevance of these rapid ...
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Contents
XXXI | 37 |
XXXV | 39 |
XXXVI | 40 |
XXXVII | 41 |
XXXIX | 42 |
XL | 43 |
XLI | 44 |
XLII | 47 |
CLXVII | 242 |
CLXIX | 243 |
CLXXVI | 244 |
CLXXVIII | 245 |
CLXXX | 246 |
CLXXXII | 247 |
CLXXXIV | 251 |
CLXXXV | 252 |
XLIV | 51 |
XLV | 53 |
XLVI | 55 |
XLVIII | 56 |
XLIX | 57 |
LI | 58 |
LIV | 59 |
LV | 60 |
LVI | 61 |
LVIII | 65 |
LIX | 71 |
LX | 72 |
LXII | 76 |
LXIV | 78 |
LXV | 79 |
LXVI | 80 |
LXVII | 81 |
LXVIII | 82 |
LXXI | 83 |
LXXIII | 84 |
LXXV | 86 |
LXXVII | 87 |
LXXX | 90 |
LXXXI | 91 |
LXXXII | 92 |
LXXXIII | 99 |
LXXXV | 101 |
LXXXVI | 102 |
LXXXVII | 103 |
LXXXVIII | 104 |
LXXXIX | 105 |
XC | 107 |
XCIII | 108 |
XCV | 109 |
XCVI | 110 |
XCVII | 111 |
XCVIII | 114 |
CI | 116 |
CII | 118 |
CIV | 120 |
CV | 129 |
CVI | 133 |
CVII | 137 |
CVIII | 138 |
CIX | 139 |
CX | 142 |
CXI | 143 |
CXII | 144 |
CXIII | 145 |
CXVII | 146 |
CXVIII | 147 |
CXX | 148 |
CXXI | 152 |
CXXIII | 154 |
CXXV | 155 |
CXXVI | 156 |
CXXVII | 157 |
CXXIX | 158 |
CXXXI | 159 |
CXXXV | 161 |
CXXXVI | 163 |
CXXXVIII | 164 |
CXLIII | 165 |
CXLV | 166 |
CXLVI | 167 |
CXLVII | 168 |
CL | 169 |
CLII | 170 |
CLIII | 173 |
CLIV | 175 |
CLVI | 177 |
CLVII | 189 |
CLVIII | 223 |
CLIX | 227 |
CLX | 229 |
CLXIII | 238 |
CLXXXVI | 253 |
CLXXXVII | 254 |
CLXXXVIII | 255 |
CXCII | 257 |
CXCIII | 258 |
CXCIV | 260 |
CXCVII | 261 |
CXCVIII | 263 |
CC | 264 |
CCI | 265 |
CCIV | 267 |
CCV | 268 |
CCVII | 269 |
CCVIII | 270 |
CCIX | 279 |
CCXI | 353 |
CCXII | 357 |
CCXIII | 359 |
CCXV | 364 |
CCXVII | 365 |
CCXVIII | 367 |
CCXIX | 368 |
CCXX | 371 |
CCXXI | 373 |
CCXXII | 374 |
CCXXIII | 375 |
CCXXV | 376 |
CCXXVI | 377 |
CCXXVII | 378 |
CCXXVIII | 379 |
CCXXX | 380 |
CCXXXII | 382 |
CCXXXIII | 383 |
CCXXXVII | 385 |
CCXXXVIII | 387 |
CCXXXIX | 388 |
CCXLI | 389 |
CCXLII | 390 |
CCXLIII | 391 |
401 | |
CCXLV | 405 |
CCXLVI | 407 |
CCXLVIII | 409 |
CCLI | 411 |
CCLII | 412 |
CCLIII | 413 |
CCLIV | 414 |
CCLV | 415 |
CCLVI | 416 |
CCLVII | 417 |
CCLIX | 418 |
CCLX | 419 |
CCLXI | 424 |
CCLXII | 425 |
CCLXIII | 428 |
CCLXIV | 429 |
CCLXV | 431 |
CCLXVI | 432 |
CCLXVII | 433 |
CCLXVIII | 439 |
CCLXX | 477 |
CCLXXII | 511 |
CCLXXIII | 515 |
CCLXXIV | 517 |
CCLXXV | 519 |
CCLXXVI | 521 |
CCLXXVII | 524 |
CCLXXVIII | 527 |
CCLXXX | 529 |
CCLXXXII | 531 |
CCLXXXIV | 545 |
CCLXXXVI | 559 |
CCLXXXVIII | 563 |
CCXC | 565 |
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Common terms and phrases
aerosol aerosol forcing albedo analysis anomalies anthropogenic AOGCM areas Assessment atmospheric CO2 average biogeochemical carbon cycle century Chapter circulation model Clim climate change climate models climate sensitivity climate system climate variability cloud CO₂ convection coupled models decades decrease distribution dynamics ecosystems effects El Niño-Southern Oscillation emission scenarios ENSO estimates experiments feedbacks Figure flux adjustment Geophys glaciers global climate global mean temperature global warming greenhouse gases GtC/yr GWPS high latitudes ice sheet increase interannual IPCC land land-surface marine Meteorological methane natural variability North Atlantic Northern Hemisphere observed ocean models Pacific parametrization patterns ppmv precipitation processes projections radiation radiative forcing rainfall range recent Research response scale sea ice sea level change sea level rise Section simulations soil moisture solar spatial stabilisation stratospheric studies sulphate aerosols surface air temperature temperature change terrestrial thermohaline circulation time-scales trends tropical tropospheric ozone uncertainties variations water vapour Wigley