Comprehensive analysis of the climate variability in the eastern Mediterranean. Part I: map-pattern classification

被引:53
作者
Kostopoulou, E.
Jones, P. D.
机构
[1] Univ E Anglia, Climat Res Unit, Norwich NR4 7TJ, Norfolk, England
[2] Natl Observ Athens, Athens, Greece
关键词
circulation patterns; rotated principal component analysis (RPCA); loading threshold; eastern Mediterranean; PRINCIPAL COMPONENT ANALYSIS; WEATHER-TYPE CLASSIFICATION; SYNOPTIC CONDITIONS; DAILY RAINFALL; ATMOSPHERIC CIRCULATION; OBJECTIVE CLIMATOLOGY; AIR-TEMPERATURE; SOUTHERN GREECE; PRECIPITATION; WINTER;
D O I
10.1002/joc.1467
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper provides an extended study of the dominant daily circulation patterns governing the climate variability in the eastern Mediterranean. The methodology adopted to determine the circulation patterns is based on combined analysis of the spatial and temporal variation of rotated principal components of sea-level pressure. A catalogue of characteristic seasonal composites is presented and discussed. It is found that, during winter and spring, large scale features situated in northern Europe affect the atmospheric circulation over the domain of study, whereas the Atlantic (Azores) anticyclone and the Asian Thermal Low define most of the observed circulation types in summer. In autumn, the area exhibits a rapid transition from the warm to cold season showing climatic features from both extreme seasons. Similarities between winter and spring/autumn patterns are detected and correlation analyses are employed between their spatial patterns to reveal that similar circulation patterns occur amongst the three seasons, which usually appear more pronounced during winter. Frequencies and trends of the proposed circulation types are examined for each season. A linear trend analysis for the overall period (1958-2000) exhibits a significant increase in the anticyclonic types particularly in winter. With respect to the cyclonic types, statistically significant negative trends have been found in all seasons especially for types associated with depressional activity in central the Mediterranean. Copyright (C) 2007 Royal Meteorological Society
引用
收藏
页码:1189 / 1214
页数:26
相关论文
共 112 条
[1]  
ALPERT P, 1990, J CLIMATE, V3, P1474, DOI 10.1175/1520-0442(1990)003<1474:IVOCTI>2.0.CO
[2]  
2
[3]  
Alpert P., 1990, Tellus, Series A (Dynamic Meteorology and Oceanography), V42A, P65, DOI 10.1034/j.1600-0870.1990.00007.x
[4]  
[Anonymous], MAPAS TIEMPO FUNDAME
[5]  
[Anonymous], THESIS U DIJON DIJON
[6]  
[Anonymous], 4 C PROB STAT ATM SC
[7]  
ARSENIPAPADIMIT.A, 1988, RIV METEOROLOGIA AER, V48, P131
[8]  
BARRING L, 1987, J CLIMATOL, V7, P267, DOI 10.1002/joc.3370070306
[9]  
Barry R., 1999, Atmosphere, weather, and climate, VEighth
[10]   THE HORIZONTAL AND VERTICAL EXTENSION OF THE PERSIAN GULF PRESSURE TROUGH [J].
BITAN, A ;
SAARONI, H .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 1992, 12 (07) :733-747