SPATIAL AND TEMPORAL SEA-SURFACE TEMPERATURE COVARIANCES IN THE MEDITERRANEAN

被引:30
作者
BARTZOKAS, A [1 ]
GANAS, IS [1 ]
机构
[1] UNIV IOANNINA, PROBABIL STAT & OPERAT RES UNIT, PROBABIL STAT & OPERAT RES UNIT, GR-45110 IOANNINA, GREECE
关键词
MEDITERRANEAN; SEA-SURFACE TEMPERATURE; PRINCIPAL COMPONENTS FACTOR ANALYSIS;
D O I
10.1002/joc.3370140206
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Using sea-surface temperature data for the, post-war period, the Mediterranean Sea is divided objectively (principal components factor analysis) into subareas with similar covariances. This division is not the same in every season of the year. In summer, two subareas are found, the west and the east. In spring and autumn three, and in winter four significant subareas denote physical oceanographic and meteorological processes. The scores of the analyses show clearly the minimum of the late 1970s and then the warming of recent years somewhat delayed in the eastern Mediterranean.
引用
收藏
页码:201 / 213
页数:13
相关论文
共 54 条
  • [41] ROTATION OF PRINCIPAL COMPONENTS
    RICHMAN, MB
    [J]. JOURNAL OF CLIMATOLOGY, 1986, 6 (03): : 293 - 335
  • [42] RICHMAN MB, 1981, J APPL METEOROL, V20, P1145, DOI 10.1175/1520-0450(1981)020<1145:ORPCAI>2.0.CO
  • [43] 2
  • [44] ROGERS JC, 1990, J CLIMATE, V3, P1364, DOI 10.1175/1520-0442(1990)003<1364:POLFMS>2.0.CO
  • [45] 2
  • [46] RUMMEL RJ, 1970, APPLIED FACTOR ANAL
  • [47] THURSTON GD, 1985, J CLIM APPL METEOROL, V24, P1245, DOI 10.1175/1520-0450(1985)024<1245:AMAOMI>2.0.CO
  • [48] 2
  • [49] WALLACE JM, 1981, MON WEATHER REV, V109, P784, DOI 10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO
  • [50] 2