Tyndall Centre Publications

@article{1153,

title = {Climate change - Regional warming and malaria resurgence},

author = {JA Patz and M Hulme and C Rosenzweig and Mitchell T. and RA Goldberg and AK Githeko and S Lele and AJ McMichael and D Le Sueur},

year  = {2002},

date = {2002-01-01},

journal = {Nature},

volume = {420},

number = {6916},

pages = {627-628},

chapter = {627},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{1040,

title = {Climate data for political areas},

author = {Mitchell T. and M Hulme},

year  = {2002},

date = {2002-01-01},

journal = {Area},

volume = {34},

pages = {109-112},

chapter = {109},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{605,

title = {Climate Policy and Development: Flexible Instruments and Developing Countries by A. Michaelowa and M. Dutschke (eds)},

author = {E Corbera},

year  = {2002},

date = {2002-01-01},

journal = {Environmental Politics},

volume = {11},

number = {4},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{511,

title = {Climate-induced oceanic oxygen fluxes: Implications for the contemporary carbon budget},

author = {L Bopp and C Le Quéré and M Heimann and AC Manning and P Monfray},

year  = {2002},

date = {2002-01-01},

journal = {Global Biogeochemical Cycles},

number = {16},

chapter = {1022},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{632b,

title = {Consensus among many voices: articulating the European Uniontextquoterights position on climate change},

author = {S Dessai and E Powroslo},

year  = {2002},

date = {2002-01-01},

journal = {Golden Gate University Law Review},

volume = {32},

pages = {351-414},

chapter = {351},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{940b,

title = {Consensus among many voices: articulating the European Uniontextquoterights position on climate change.},

author = {N Lacasta and S Dessai},

year  = {2002},

date = {2002-01-01},

journal = {Golden Gate University Law Review},

volume = {32},

pages = {351-414},

chapter = {351},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{448b,

title = {The consequences of CO2 stabilisation for the impacts of climate change},

author = {N W Arnell and M Cannell and M Hulme and S Kovats and JFB Mitchell and R J Nicholls and M Parry and M Livermore and A White},

year  = {2002},

date = {2002-01-01},

journal = {Climatic Change},

volume = {53},

pages = {413-446},

chapter = {413},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{894,

title = {Decarbonising the UK: A textquoteleftRadical Agendatextquoteright from the Cabinet Office?},

author = {Jordan A},

year  = {2002},

date = {2002-01-01},

journal = {Political Quarterly},

volume = {73},

number = {3},

pages = {344-352},

chapter = {344},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{1189,

title = {A dirty planet is a happy planet},

author = {A Ridgwell},

year  = {2002},

date = {2002-01-01},

journal = {Planet Earth NERC},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{1188,

title = {Does the ocean iron cycle destabilize the glacial climate system?},

author = {A Ridgwell},

year  = {2002},

date = {2002-01-01},

journal = {Geochimica Et Cosmochimica Acta.},

volume = {66},

number = {15A},

pages = {A639},

chapter = {A639},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{1184,

title = {Dust in the Earth system: The biogeochemical linking of land, air and sea},

author = {A Ridgwell},

year  = {2002},

date = {2002-01-01},

journal = {Philosophical Transactions of the Royal Society A},

volume = {360},

number = {1801},

pages = {2905-2924},

chapter = {2905},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{1138,

title = {Evidence for trends in heavy rainfall events over the UK},

author = {Tim Osborn and M Hulme},

year  = {2002},

date = {2002-01-01},

journal = {Philosophical Transactions of the Royal Society of London Series a-Mathematical Physical and Engineering Sciences},

volume = {360},

number = {1796},

pages = {1313-1325},

chapter = {1313},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{991,

title = {An exploration of regional climate change scenarios for Scotland},

author = {X Lu and M Hulme},

year  = {2002},

date = {2002-01-01},

journal = {Scottish Geographical Journal},

volume = {117},

pages = {251-270},

chapter = {251},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{e7edcc0a26ba4a239305e567a9751e80,

title = {Trends of extreme temperatures in Europe and China based on daily observations},

author = {Z Yan and PD Jones and TD Davies and A Moberg and H Bergström and D Camuffo and C Cocheo and M Maugeri and GR Demarée and T Verhoeve and E Thoen and M Barriendos and R Rodríguez and J Martín-Vide and C Yang},

doi = {10.1023/A:1014939413284},

issn = {0165-0009},

year  = {2002},

date = {2002-01-01},

journal = {Climatic Change},

volume = {53},

number = {1/3},

pages = {355–392},

publisher = {Springer},

abstract = {Ten of the longest daily temperature series presently available in Europe and China are analysed, focusing on changes in extremes since pre-industrial times. We consider extremes in both a relative (with respect to the time of year) and an absolute sense. To distinguish changes in extremes from changes affecting the main part of the temperature distribution, a percentile smaller than 10 (and/or larger than 90) is recommended for defining an extreme. Three periods of changes in temperature extremes are identified: decreasing warm extremes before the late 19th century; decreasing cold extremes since then and increasing warm extremes since the 1960s. The early decreases and recent increases of warm extremes dominate in summer, while the decrease of cold extremes for winter persists throughout the whole period. There were more frequent combined (warm plus cold) extremes during the 18th century and the recent warming period since 1961 at most of the ten stations, especially for summer. Since 1961, the annual frequency of cold extremes has decreased by about 7% per century with warm extremes increasing by more than 10% per century but with large spatial variability. Compared with recent annual mean warming of about 2-3°C/century, the coldest winter temperatures have increased at three times this rate, causing a reduced within-season range and therefore less variable winters. Changes in the warmest summer temperatures since 1961 exhibit large spatial variability, with rates of change ranging from slightly negative to 6°C/century. More extensive station observations since 1961 indicate that the single site results are representative of larger regions, implying also that the extremes studied are the result of large-scale changes. Recent circulation changes in daily gridded pressure data, used as an indicator of wind speed changes, support the results by explaining some of the trends.},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{1186,

title = {Feedback between aeolian dust, climate and atmospheric CO2 in glacial time},

author = {A Ridgwell and AJ Watson},

year  = {2002},

date = {2002-01-01},

journal = {Paleoceanography},

volume = {17},

number = {4},

pages = {1059},

chapter = {1059},

keywords = {},

pubstate = {published},

tppubtype = {article}

}