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91探花
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Professor Myles Allen CBE FRS

Statutory Professor

Research theme

  • Climate physics

Sub department

  • Atmospheric, Oceanic and Planetary Physics
Myles.Allen@physics.ox.ac.uk
Telephone: 01865 (2)72085,01865 (2)75895
Atmospheric Physics Clarendon Laboratory, room 109
  • About
  • Publications

Impact of delay in reducing carbon dioxide emissions

Nature Climate Change Springer Nature 4:1 (2014) 23-26

Authors:

Myles R Allen, Thomas F Stocker

THE HEAVY PRECIPITATION EVENT OF MAY-JUNE 2013 IN THE UPPER DANUBE AND ELBE BASINS

BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY 95:9 (2014) S69-S72

Authors:

Nathalie Schaller, Friederike EL Otto, Geert Jan van Oldenborgh, Neil R Massey, Sarah Sparrow, Myles R Allen

The role of short-lived climate pollutants in meeting temperature goals

Nature Climate Change 3:12 (2013) 1021-1024

Authors:

NHA Bowerman, DJ Frame, C Huntingford, JA Lowe, SM Smith, MR Allen

Abstract:

Some recent high-profile publications have suggested that immediately reducing emissions of methane, black carbon and other short-lived climate pollutants (SLCPs) may contribute substantially towards the goal of limiting global warming to 2C above pre-industrial levels. Although this literature acknowledges that action on long-lived climate pollutants (LLCPs) such as CO 2 is also required, it is not always appreciated that SLCP emissions in any given decade only have a significant impact on peak temperature under circumstances in which CO 2 emissions are falling. Immediate action on SLCPs might potentially 'buy time' for adaptation by reducing near-term warming; however early SLCP reductions, compared with reductions in a future decade, do not buy time to delay reductions in CO 2. 漏 2013 Macmillan Publishers Limited. All rights reserved.

Breaks in trends

Nature Geoscience Springer Nature 6:12 (2013) 992-993

Authors:

Felix Pretis, Myles Allen

Constraining the ratio of global warming to cumulative CO2 emissions using CMIP5 simulations

Journal of Climate 26:18 (2013) 6844-6858

Authors:

NP Gillett, VK Arora, D Matthews, MR Allen

Abstract:

The ratio of warming to cumulative emissions of carbon dioxide has been shown to be approximately independent of time and emissions scenarios and directly relates emissions to temperature. It is therefore a potentially important tool for climate mitigation policy. The transient climate response to cumulative carbon emissions (TCRE), defined as the ratio of global-mean warming to cumulative emissions at CO2 doubling in a 1%yr-1 CO2 increase experiment, ranges from 0.8 to 2.4K EgC-1 in 15 models from phase 5 of the Coupled Model Intercomparison Project (CMIP5)-a somewhat broader range than that found in a previous generation of carbon-climate models. Using newly available simulations and a new observational temperature dataset to 2010, TCREis estimated from observations by dividing an observationally constrained estimate of CO2-attributable warming by an estimate of cumulative carbon emissions to date, yielding an observationally constrained 5%-95% range of 0.7-2.0K EgC-1. 漏 2013 American Meteorological Society.

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