Do weak AR4 models bias projections of future climate changes over Australia?

被引:36
作者
Perkins, S. E. [1 ]
Pitman, A. J. [1 ]
机构
[1] Univ New S Wales, Climate Change Res Ctr, Sydney, NSW 2052, Australia
关键词
TEMPERATURE EVENTS; EXTREMES; VARIABILITY; PRECIPITATION; UNCERTAINTY; FREQUENCY; WILL;
D O I
10.1007/s10584-008-9502-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Regional climate projections using climate models commonly use an "all-model" ensemble based on data sets such as the Intergovernmental Panel on Climate Change's (IPCC) 4th Assessment (AR4). Some regional assessments have omitted models based on specific criteria. We use a criteria based on the capacity of climate models to simulate the observed probability density function calculated using daily data, model-by-model and region-by-region for each of the AR4 models over Australia. We demonstrate that by omitting those climate models with relatively weak skill in simulating the observed probability density functions of maximum and minimum temperature and precipitation, different regional projections are obtained. Differences include: larger increases in the mean maximum and mean minimum temperatures, but smaller increases in the annual maximum and minimum temperatures. There is little impact on mean precipitation but the better models simulate a larger increase in the annual rainfall event combined with a larger decrease in the number of rain days. The weaker models bias the amount of mean warming towards lower increases, bias annual maximum temperatures to excessive warming and bias precipitation such that the amount of the annual rainfall event is under-estimated. We suggest that omitting weak models from regional scale estimates of future climate change helps clarify the nature and scale of the projected impacts of global warming.
引用
收藏
页码:527 / 558
页数:32
相关论文
共 34 条
[1]  
[Anonymous], ATLAS AUSTR RESOURCE
[2]  
[Anonymous], CLIM CHANG 2007
[3]  
[Anonymous], 2007, AR4 CLIM CHANG 2007
[4]   Where will species go? Incorporating new advances in climate modelling into projections of species distributions [J].
Beaumont, Linda J. ;
Pitman, A. J. ;
Poulsen, Michael ;
Hughes, Lesley .
GLOBAL CHANGE BIOLOGY, 2007, 13 (07) :1368-1385
[5]  
Colombo AF, 1999, J CLIMATE, V12, P2490, DOI 10.1175/1520-0442(1999)012<2490:CVATFO>2.0.CO
[6]  
2
[7]   Climate extremes: Observations, modeling, and impacts [J].
Easterling, DR ;
Meehl, GA ;
Parmesan, C ;
Changnon, SA ;
Karl, TR ;
Mearns, LO .
SCIENCE, 2000, 289 (5487) :2068-2074
[8]  
Forster P, 2007, AR4 CLIMATE CHANGE 2007: THE PHYSICAL SCIENCE BASIS, P129
[9]   Change in mean temperature as a predictor of extreme temperature change in the Asia-Pacific region [J].
Griffiths, GM ;
Chambers, LE ;
Haylock, MR ;
Manton, MJ ;
Nicholls, N ;
Baek, HJ ;
Choi, Y ;
Della-Marta, PM ;
Gosai, A ;
Iga, N ;
Lata, R ;
Laurent, V ;
Maitrepierre, L ;
Nakamigawa, H ;
Ouprasitwong, N ;
Solofa, D ;
Tahani, L ;
Thuy, DT ;
Tibig, L ;
Trewin, B ;
Vediapan, K ;
Zhai, P .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2005, 25 (10) :1301-1330
[10]   GREENHOUSE WARMING AND THRESHOLD TEMPERATURE EVENTS IN VICTORIA, AUSTRALIA [J].
HENNESSY, KJ ;
PITTOCK, AB .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 1995, 15 (06) :591-612