External control of 20th century temperature by natural and anthropogenic forcings.
By P. Stott, S. Tett, G. Jones, Myles Allen, Johnny Mitchell, G. Jenkins. Science, 2000
698 citations recorded by the source corpus.
Subfields: Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/adc89b5f7b6a4b455ee6822c365be4a62049b6d1
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In Global and Planetary Change
- Reto Knutti
- M. Lockwood
- Piers M. Forster
- Gerald A. Meehl
- J. Gregory
- Peter M. Caldwell
- M. Webb
- D. Shindell
Citations in the corpus
- Behavior of tropopause height and atmospheric temperature in models, reanalyses, and observations: Decadal changes (2003, background): “…this work has focused on either surface temperature [ Santer et al. , 1995; Hegerl et al. , 1996, 1997; Wigley et al. , 1998; Tett et al. , 1999; Stott et al. , 2000; Allen et al. , 2002] or on zonally averaged temperatures in the free atmosphere [ Karoly et al. , 1994; Santer et al. , 1996b;…”
- Evaluation of remote sensing based terrestrial productivity from MODIS using regional tower eddy flux network observations (2006, background): “Additionally, it is impossible to account for associated climate change, such as increases in air temperature without considering the effects of human activity on the carbon cycle [2].”
- Tropospheric O3 moderates responses of temperate hardwood forests to elevated CO2: a synthesis of molecular to ecosystem results from the Aspen FACE project (2003, background): “Current climate change scenarios predict further increases in atmospheric CO 2 (Stott et al .”
- Estimating signal amplitudes in optimal fingerprinting, part I: theory (2003, background): “Stevens and North 1996; Wigley et al. 1997; North and Stevens 1998; Knutti et al. 2002).”
- Detection of volcanic, solar and greenhouse gas signals in paleo‐reconstructions of Northern Hemispheric temperature (2003, background): “A similar tendency occurs in coupled climate models, [e.g., Stott et al., 2000].”
- Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data (2005, methodology): “has been caused by natural forcing factors alone, as model experiments that use natural-only forcings fail to reproduce this warmin”
- Are there connections between the Earth's magnetic field and climate? (2007, background): “This conclusion agrees with numerical modelling studies indicating that the rise in the content of atmospheric greenhouse gases is very probably the main cause of the significant warming observed during the last three decades (Stott et al., 2000; Meehl et al., 2004).”
- Separating signal and noise in atmospheric temperature changes: The importance of timescale (2011, methodology): “…in the spatial pattern and/or the temporal evolution of signal and noise [e.g., Hasselmann, 1979, 1993; Santer et al., 1994, 1995, 1996; North et al., 1995; Tett et al., 1996; Hegerl et al., 1996, 2007; Allen and Tett, 1999; Stott et al., 2000; Barnett et al., 2001, 2005; Gillett et al., 2002].”
- Climate predictability on interannual to decadal time scales: the initial value problem (2002, methodology): “The top four " rows " represent the four independent realisations of 20th century climate simulated by Stott et al (2000).”
- Solar radiative output and its variability: evidence and mechanisms (2004, background): “Reliable knowledge of solar-induced variations is essential for understanding and attribution of anthropogenic in uences on Earth's climate (Stott et al., 2000) and changes of the ozone layer in the stratosphere (e.g. Geller and Smyshlyaev, 2002).”
- Anthropogenic alterations of genetic diversity within tree populations: Implications for forest ecosystem resilience (2008, background): “…increased environmental stress exposure) that may result from unfettered l., 1999; Likens et al., 1996; Nilsson, 2000; Schaberg et al., 2001; Stott et al., 2000; relationship between genetic diversity and various fitness measures (e.g., Knowles and Grant, 1981; Mitton et al., 1981; Neale…”
- Solar Influence on Global and Regional Climates (2012, background): “The bottom panel shows that the response to anthropogenic effects is widespread and particularly strong in the northern hemisphere at middle to high latitudes, as predicted by GCMs (e.g., Stott et al. 2000).”
- Initial steps of aerosol growth (2004, neutral): “In the global troposphere aerosol particles are thought to contribute to climate change patterns (Stott et al., 2000; Ramanathan et al., 2001; Yu et al., 2001; Sekiguchi et al., 2003).”