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. |
From inside the book
Results 6-10 of 86
Page 30
... variability or extreme weather events . Some reports have already suggested an increase in variability or extremes has taken place in recent decades . Do meteorological records support this ? There are inadequate data to determine ...
... variability or extreme weather events . Some reports have already suggested an increase in variability or extremes has taken place in recent decades . Do meteorological records support this ? There are inadequate data to determine ...
Page 33
... variability on a wide range of time- and space - scales which is broadly comparable to that observed . This " natural " variability arises from the internal processes at work in the climate system and not from changes in external ...
... variability on a wide range of time- and space - scales which is broadly comparable to that observed . This " natural " variability arises from the internal processes at work in the climate system and not from changes in external ...
Page 35
... variability " . The report went on to explain that " the observed increase could be largely due to this natural variability ; alternatively this variability and other human factors could have offset a still larger human - induced ...
... variability " . The report went on to explain that " the observed increase could be largely due to this natural variability ; alternatively this variability and other human factors could have offset a still larger human - induced ...
Page 36
... variability or the volcanic aerosol loading of the atmosphere . It is difficult to separate a signal from the noise of natural variability in the observations . This is because there are large uncertainties in the evolution and ...
... variability or the volcanic aerosol loading of the atmosphere . It is difficult to separate a signal from the noise of natural variability in the observations . This is because there are large uncertainties in the evolution and ...
Page 37
Sorry, this page's content is restricted.
Sorry, this page's content is restricted.
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 |
Other editions - View all
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