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J. A. Kettleborough

Researcher at Rutherford Appleton Laboratory

Publications -  5
Citations -  1605

J. A. Kettleborough is an academic researcher from Rutherford Appleton Laboratory. The author has contributed to research in topics: Climate model & Climate change. The author has an hindex of 4, co-authored 4 publications receiving 1548 citations.

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Uncertainty in predictions of the climate response to rising levels of greenhouse gases.

TL;DR: Results from the ‘climateprediction.net’ experiment are presented, the first multi-thousand-member grand ensemble of simulations using a general circulation model and thereby explicitly resolving regional details, finding model versions as realistic as other state-of-the-art climate models but with climate sensitivities ranging from less than 2 K to more than 11’K.
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Origins and estimates of uncertainty in predictions of twenty-first century temperature rise

TL;DR: It is found that, in the absence of policies to mitigate climate change, global-mean temperature rise is insensitive to the differences in the emissions scenarios over the next four decades and that in the future, as the signal of climate change emerges further, the predictions will become better constrained.
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Distributed computing for public-interest climate modeling research

TL;DR: The CLIMATEPREDICTION.COM project has developed the software necessary to carry out such a project in the public domain this article, along with the computational challenges such as data mining, visualization, and distributed database management.
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Estimates of Uncertainty in Predictions of Global Mean Surface Temperature

TL;DR: In this article, a method for estimating uncertainty in future climate change is discussed in detail and applied to predictions of global mean temperature change, using optimal fingerprinting to make estimates of uncertainty in model simulations of twentieth-century warming.
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Predictability of European winter 2020/2021: Influence of a mid‐winter sudden stratospheric warming

TL;DR: In this article , the forecast ensemble mean was shifted towards a positive NAO phase by a negative North Atlantic Oscillation (NAO) index, which was captured within the ensemble spread of predictions from the Met Office Global Seasonal forecast system.