globalchange  > 过去全球变化的重建
DOI: 10.1007/s00382-012-1571-1
Scopus记录号: 2-s2.0-84869500561
论文题名:
A step-response approach for predicting and understanding non-linear precipitation changes
作者: Good P.; Ingram W.; Lambert F.H.; Lowe J.A.; Gregory J.M.; Webb M.J.; Ringer M.A.; Wu P.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2012
卷: 39, 期:12
起始页码: 2789
结束页码: 2803
语种: 英语
英文关键词: Global climate change ; Impacts ; Precipitation ; Projections
英文摘要: Future changes in precipitation represent one of the most important and uncertain possible effects of future climate change. We demonstrate a new approach based on idealised CO2 step-change general circulation model (GCM) experiments, and test it using the HadCM3 GCM. The approach has two purposes: to help understand GCM projections, and to build and test a fast simple model for precipitation projections under a wide range of forcing scenarios. Overall, we find that the CO2 step experiments contain much information that is relevant to transient projections, but that is more easily extracted due to the idealised experimental design. We find that the temporary acceleration of global-mean precipitation in this GCM following CO2 ramp-down cannot be fully explained simply using linear responses to CO2 and temperature. A more complete explanation can be achieved with an additional term representing interaction between CO2 and temperature effects. Energy budget analysis of this term is dominated by clear-sky outgoing long-wave radiation (CSOLR) and sensible heating, but cloud and short-wave terms also contribute. The dominant CSOLR interaction is attributable to increased CO2 raising the mean emission level to colder altitudes, which reduces the rate of increase of OLR with warming. This behaviour can be reproduced by our simple model. On regional scales, we compare our approach with linear 'pattern-scaling' (scaling regional responses by global-mean temperature change). In regions where our model predicts linear change, pattern-scaling works equally well. In some regions, however, substantial deviations from linear scaling with global-mean temperature are found, and our simple model provides more accurate projections. The idealised experiments reveal a complex pattern of non-linear behaviour. There are likely to be a range of controlling physical mechanisms, different from those dominating the global-mean response, requiring focussed investigation for individual regions, and in other GCMs. © 2012 Crown Copyright.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/55098
Appears in Collections:过去全球变化的重建

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作者单位: Met Office Hadley Centre, Exeter, United Kingdom; Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, Oxford, United Kingdom; College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom; Department of Meteorology, Walker Institute for Climate System Research, University of Reading, Reading, United Kingdom

Recommended Citation:
Good P.,Ingram W.,Lambert F.H.,et al. A step-response approach for predicting and understanding non-linear precipitation changes[J]. Climate Dynamics,2012-01-01,39(12)
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