Climatic forcing of droughts:: a Central European example

被引:20
作者
Pongrácz, R
Bogardi, I
Duckstein, L
机构
[1] Eotvos Lorand Univ, Dept Meteorol, H-1117 Budapest, Hungary
[2] Univ Nebraska, Dept Civil Engn, Lincoln, NE 68588 USA
[3] Ecole Natl Genie Rural Eaux & Forets, F-75732 Paris 15, France
来源
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES | 2003年 / 48卷 / 01期
关键词
Palmer Drought Severity Index; fuzzy logic; fuzzy rule-based modelling; El Nino Southern Oscillation; Southern Oscillation Index; circulation patterns; drought;
D O I
10.1623/hysj.48.1.39.43480
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
A fuzzy rule-based technique is used for modelling the relationship between climatic forcing and droughts in a Central/Eastern European country, Hungary. Two types of climatic forcing-called premises-are considered: atmospheric circulation patterns (CP) and El Nino Southern Oscillation (ENSO). Both the Hess-Brezowsky CP types and ENSO events influence the occurrence of droughts, but the ENSO signal is relatively weak in a statistical sense. The fuzzy rule-based approach is able to learn the high space-time variability of monthly Palmer Drought Severity Index (PDSI) and results in a proper reproduction of the empirical frequency distributions. The "engine" of the approach, the fuzzy rules, are ascertained from a subset called the learning set of the observed time series of premises (monthly CP frequencies and Southern Oscillation Index) and PDSI response. Then an independent subset, the validation set, is used to check how the application of fuzzy rules reproduces the observed PDSI.
引用
收藏
页码:39 / 50
页数:12
相关论文
共 46 条
[31]  
PONGRACZ R, 2000, IDOJARAS, V104, P1
[32]   SURFACE CLIMATE AND STREAMFLOW VARIABILITY IN THE WESTERN UNITED-STATES AND THEIR RELATIONSHIP TO LARGE-SCALE CIRCULATION INDEXES [J].
REDMOND, KT ;
KOCH, RW .
WATER RESOURCES RESEARCH, 1991, 27 (09) :2381-2399
[33]   ENSO variability and atmospheric response in a global coupled atmosphere-ocean GCM [J].
Roeckner, E ;
Oberhuber, JM ;
Bacher, A ;
Christoph, M ;
Kirchner, I .
CLIMATE DYNAMICS, 1996, 12 (11) :737-754
[34]  
SCHWING F, 2000, EOS T AM GEOPHYS UN, V81, P304
[35]  
Schwing F., 2000, EOS T AM GEOPHYS UN, V81, P301, DOI DOI 10.1029/00EO00227
[36]  
SIMMONS AJ, 1988, NATO ASI SER, V2, P627
[37]   Increased El Nino frequency in a climate model forced by future greenhouse warming [J].
Timmermann, A ;
Oberhuber, J ;
Bacher, A ;
Esch, M ;
Latif, M ;
Roeckner, E .
NATURE, 1999, 398 (6729) :694-697
[38]  
Van Oldenborgh GJ, 2000, INT J CLIMATOL, V20, P565, DOI [10.1002/(SICI)1097-0088(200004)20:5<565::AID-JOC488>3.0.CO
[39]  
2-5, 10.1002/(SICI)1097-0088(200004)20:5&lt
[40]  
565::AID-JOC488&gt