The use of weather types and air flow indices for GCM downscaling

被引:74
作者
Conway, D [1 ]
Jones, PD [1 ]
机构
[1] Univ E Anglia, Ctr Res Unit, Norwich NR4 7TJ, Norfolk, England
关键词
General Circulation Model (GCM); downscaling; weather types; air flow indices;
D O I
10.1016/S0022-1694(98)00216-9
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
A variety of different methods have been proposed for downscaling large-scale General Circulation Model (GCM) output to the time and space scales required for climate impact studies. Using weather types to achieve this goal provides greater understanding of the problems that are involved compared to the many "black box" techniques that have been proposed. Analyses using Lamb weather types, counts of weather fronts and air flow indices over the British Isles show strong relationships with daily rainfall characteristics such as the probability and amount of rainfall. Three versions of a weather type method are described for generating daily rainfall series. Two methods use an objective scheme to classify daily circulation types over the British isles along the lines of Lamb's subjective classification. The third method is based on user-defined categories of vorticity. Each method categorises rainfall events according to whether the previous day was wet or dry. All three methods successfully reproduce the monthly means, persistence and interannual variability of two daily rainfall time series during a validation period. A significant advantage of using vorticity is that it is a continuous variable and is strongly related to the probability of rainfall and the magnitude of rainfall events. The paper ends with a discussion of the issues relevant to the application of this method to the development of climate scenarios from GCMs. (C) 1998 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:348 / 361
页数:14
相关论文
共 41 条
[1]  
Bardossy A, 1994, CLIMATE CHANGE, UNCERTAINTY, AND DECISION-MAKING, P33
[2]   Estimates of low frequency natural variability in near-surface air temperature [J].
Barnett, TP ;
Santer, BD ;
Jones, PD ;
Bradley, RS ;
Briffa, KR .
HOLOCENE, 1996, 6 (03) :255-263
[3]  
Barry R.G., 1973, SYNOPTIC CLIMATOLOGY
[4]  
[Carter T.R. Intergovernmental Panel on Climate Change (IPCC) Intergovernmental Panel on Climate Change (IPCC)], 1994, IPCC SPECIAL REPORT
[5]   Precipitation and air flow indices over the British Isles [J].
Conway, D ;
Wilby, RL ;
Jones, PD .
CLIMATE RESEARCH, 1996, 7 (02) :169-183
[6]   USE OF A LIMITED-AREA MODEL NESTED IN A GENERAL-CIRCULATION MODEL FOR REGIONAL CLIMATE SIMULATION OVER EUROPE [J].
GIORGI, F ;
MARINUCCI, MR ;
VISCONTI, G .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D11) :18413-18431
[7]   A 2XCO2 CLIMATE CHANGE SCENARIO OVER EUROPE GENERATED USING A LIMITED AREA MODEL NESTED IN A GENERAL-CIRCULATION MODEL .2. CLIMATE CHANGE SCENARIO [J].
GIORGI, F ;
MARINUCCI, MR ;
VISCONTI, G .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D9) :10011-10028
[8]   SIMULATION OF DAILY VARIABILITY OF SURFACE-TEMPERATURE AND PRECIPITATION OVER EUROPE IN THE CURRENT AND 2XCO(2) CLIMATES USING THE UKMO CLIMATE MODEL [J].
GREGORY, JM ;
MITCHELL, JFB .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1995, 121 (526) :1451-1476
[9]  
GREGORY JM, 1991, INT J CLIMATOL, V11, P331, DOI 10.1002/joc.3370110308
[10]  
Gyalistras Dimitrios, 1994, Climate Research, V4, P167, DOI 10.3354/cr004167