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T M L Wigley

Biographic Data

ID3755679
NAMET M L Wigley
GIVEN NAMEST M L
FAMILY NAMEWigley
SIGNATUREWIGLEY T M L
AFFILIATIONSUniversity of East Anglia
ORCID0000-0002-2882-5421
VERIFIEDYes
TOTAL WORKS8
TOTAL CITATIONS24
AUTHOR COUNT8
EDITOR COUNT0
FIRST PUBLICATION YEAR1982
LATEST PUBLICATION YEAR2011
H-INDEX2
  • Emulating coupled atmosphere-ocean and carbon cycle models with a simpler model, Magicc6 – Part 1: Model description and calibration

    Open Access•Malte Meinshausen, S C B Raper et al.•ARTICLE•Atmospheric Chemistry and Physics•2011

    Current scientific knowledge on the future response of the climate system to human-induced perturbations is comprehensively captured by various model intercomparison efforts. In the preparation of the Fourth Assessment Report (AR4) of the Intergovernmental Panel on Climate Change (IPCC), intercomparisons were organized for atmosphere-ocean general circulation models (AOGCMs) and carbon cycle models, named "CMIP3" and "C4MIP", respectively. Despit…

  • Avoiding dangerous climate change

    H J Schellnhuber, W Cramer et al.•ARTICLE•Choice Reviews Online•2006

    The impacts of climate change are already being observed in a variety of sectors and there is greater clarity that these changes are being caused by human activities, mainly through release of greenhouse gases. In 2005 the UK Government hosted the Avoiding Dangerous Climate Change conference to take an in-depth look at the scientific issues associated with climate change. This volume presents the most recent findings from the leading internationa…

  • Decadal timescale links between Antarctic Peninsula ice-core oxygen-18, deuterium and temperature

    Open Access•P D Jones, Roy Marsh et al.•ARTICLE•The Holocene•1993•Cited by: 6

    The Antarctic Peninsula region has exprienced a long-term warming trend over the twentieth century, with the 1971-90 mean at Faraday being 1.9°C warmer than the mean over 1903-41 based on expedition reports. For the period prior to 1900, there is conflicting evidence from different data sources. An initial interpretation of isotopic data from ice cores suggests that the nineteenth century was warmer than the twentieth century. In contrast, snow a…

  • Cross-dating methods in dendrochronology

    Open Access•T M L Wigley, P D Jones et al.•ARTICLE•Journal of Archaeological Science•1987•Cited by: 16•References: 1

  • Climatic Trends for Tropical Africa: A Research Report for the Overseas Development Administration

    A T Grove, G Farmer et al.•ARTICLE•Geographical Journal•1986•Cited by: 2

  • A Comparison of Evidence for Late Holocene Summer Temperature Variations in the Northern Hemisphere

    Open Access•Lawrence E Williams, L D Williams et al.•ARTICLE•Quaternary Research•1983

    Data on glacier, tree-line, tree-ring, pollen, and ice-core variations in North America, Greenland, and Europe during the last 2000 yr (up to A.D. 1800) are compared in detail on the century time scale. Only data that may be indicative of summer temperature changes are included, since these comprise most of the available paleoclimatic information, although some variations (especially of glaciers) may have been in response to precipitation changes…

  • Climatic Change and Historical Discontinuity

    John D Post, T M L Wigley et al.•ARTICLE•The Journal of Interdisciplinary…•1983

  • Warming of the climate

    Open Access•T M L Wigley•ARTICLE•Futures•1982

  • Cross-dating methods in dendrochronology

    Open Access•T M L Wigley, P D Jones et al.•ARTICLE•Journal of Archaeological Science•1987•Cited by: 16•References: 1

  • Decadal timescale links between Antarctic Peninsula ice-core oxygen-18, deuterium and temperature

    Open Access•P D Jones, Roy Marsh et al.•ARTICLE•The Holocene•1993•Cited by: 6

    The Antarctic Peninsula region has exprienced a long-term warming trend over the twentieth century, with the 1971-90 mean at Faraday being 1.9°C warmer than the mean over 1903-41 based on expedition reports. For the period prior to 1900, there is conflicting evidence from different data sources. An initial interpretation of isotopic data from ice cores suggests that the nineteenth century was warmer than the twentieth century. In contrast, snow a…

  • Climatic Trends for Tropical Africa: A Research Report for the Overseas Development Administration

    A T Grove, G Farmer et al.•ARTICLE•Geographical Journal•1986•Cited by: 2

  • Warming of the climate

    Open Access•T M L Wigley•ARTICLE•Futures•1982

  • A Comparison of Evidence for Late Holocene Summer Temperature Variations in the Northern Hemisphere

    Open Access•Lawrence E Williams, L D Williams et al.•ARTICLE•Quaternary Research•1983

    Data on glacier, tree-line, tree-ring, pollen, and ice-core variations in North America, Greenland, and Europe during the last 2000 yr (up to A.D. 1800) are compared in detail on the century time scale. Only data that may be indicative of summer temperature changes are included, since these comprise most of the available paleoclimatic information, although some variations (especially of glaciers) may have been in response to precipitation changes…

  • Climatic Change and Historical Discontinuity

    John D Post, T M L Wigley et al.•ARTICLE•The Journal of Interdisciplinary…•1983

  • Climatic Trends for Tropical Africa: A Research Report for the Overseas Development Administration

    A T Grove, G Farmer et al.•ARTICLE•Geographical Journal•1986•Cited by: 2

  • Cross-dating methods in dendrochronology

    Open Access•T M L Wigley, P D Jones et al.•ARTICLE•Journal of Archaeological Science•1987•Cited by: 16•References: 1

  • Decadal timescale links between Antarctic Peninsula ice-core oxygen-18, deuterium and temperature

    Open Access•P D Jones, Roy Marsh et al.•ARTICLE•The Holocene•1993•Cited by: 6

    The Antarctic Peninsula region has exprienced a long-term warming trend over the twentieth century, with the 1971-90 mean at Faraday being 1.9°C warmer than the mean over 1903-41 based on expedition reports. For the period prior to 1900, there is conflicting evidence from different data sources. An initial interpretation of isotopic data from ice cores suggests that the nineteenth century was warmer than the twentieth century. In contrast, snow a…

  • Avoiding dangerous climate change

    H J Schellnhuber, W Cramer et al.•ARTICLE•Choice Reviews Online•2006

    The impacts of climate change are already being observed in a variety of sectors and there is greater clarity that these changes are being caused by human activities, mainly through release of greenhouse gases. In 2005 the UK Government hosted the Avoiding Dangerous Climate Change conference to take an in-depth look at the scientific issues associated with climate change. This volume presents the most recent findings from the leading internationa…

  • Emulating coupled atmosphere-ocean and carbon cycle models with a simpler model, Magicc6 – Part 1: Model description and calibration

    Open Access•Malte Meinshausen, S C B Raper et al.•ARTICLE•Atmospheric Chemistry and Physics•2011

    Current scientific knowledge on the future response of the climate system to human-induced perturbations is comprehensively captured by various model intercomparison efforts. In the preparation of the Fourth Assessment Report (AR4) of the Intergovernmental Panel on Climate Change (IPCC), intercomparisons were organized for atmosphere-ocean general circulation models (AOGCMs) and carbon cycle models, named "CMIP3" and "C4MIP", respectively. Despit…

Climate change (6 works) · Geography (6 works) · Geology (6 works) · Geology (6 works) · Climatology (5 works) · Oceanography (4 works) · Oceanography (4 works) · Tree-ring climate responses (3 works) · Climate Change, Adaptation, Migration (2 works) · Dendrochronology (2 works)

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