Synoptic regimes associated with the eastern Mediterranean wet season cyclone tracks

被引:31
作者
Almazroui, Mansour [1 ]
Awad, Adel M. [1 ]
机构
[1] King Abdulaziz Univ, Dept Meteorol, Ctr Excellence Climate Change Res, POB 80234, Jeddah 21589, Saudi Arabia
关键词
East Mediterranean; Cyclone tracks; Cyclogenesis and effectiveness areas; Cyclone regimes; Track classification; WEST AFRICAN DEPRESSIONS; OBJECTIVE CLIMATOLOGY; SURFACE CYCLONES; FLOW PATTERNS; NORTH-AFRICA; VARIABILITY; MODEL; CYCLOGENESIS; CIRCULATION; REGION;
D O I
10.1016/j.atmosres.2016.05.015
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The main synoptic patterns associated with the wet season (October May) eastern Mediterranean cyclones have been analyzed and described using NCEP/NCAR reanalysis datasets for the period 1958-2013. The cyclone tracks detected in the eastern Mediterranean are classified into two types based on their positions: the local tracks and the long tracks. The local tracks are either stationary or short tracks. The long tracks distinguished into eleven very closed and highly correlated clusters, which are presented into three regimes namely the northern, the southern and the eastern border Mediterranean regimes. Among the 940 (44.78% of a total of 2099) long tracks, the northern, southern, and eastern border regime contributes respectively about 53.62%, 41.81% and 5% of the long tracks. In addition, the distribution of the long tracks reveals that a larger proportion of the cyclones are generated at the northern coast during November and spring months, while few cyclones are developed over the eastern Mediterranean border in warm months (April and May). Further, their synoptic features show that the regimes are associated with the extension of Azores high, specifically for each regime, the cyclogenesis areas of its clusters are controlled by the intersection of low level (850 hPa) trough and the position of the upper level (250 hPa) maximum wind. Furthermore, the orientations of clusters are controlled by the extension of Siberian high and the shape of cyclonic trough at 850 hPa. In addition, the synoptic study shows that most of the southern cyclones generated externally by African and Red Sea troughs, while most of the northern and eastern border cyclones are generated internally. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:92 / 118
页数:27
相关论文
共 69 条
[1]  
Ahrens C.D., 2009, Meteorology Today: An Introduction to Weather, Climate, and the environment, Vninth
[2]   A climatological study: wet season cyclone tracks in the East Mediterranean region [J].
Almazroui, Mansour ;
Awad, Adel M. ;
Islam, M. Nazrul ;
Al-Khalaf, A. K. .
THEORETICAL AND APPLIED CLIMATOLOGY, 2015, 120 (1-2) :351-365
[3]  
ALPERT P, 1990, J CLIMATE, V3, P1474, DOI 10.1175/1520-0442(1990)003<1474:IVOCTI>2.0.CO
[4]  
2
[5]  
Alpert P., 1990, Tellus, Series A (Dynamic Meteorology and Oceanography), V42A, P65, DOI 10.1034/j.1600-0870.1990.00007.x
[6]  
[Anonymous], 2007, Adv. Geosci., DOI [10.5194/adgeo-12-59-2007, DOI 10.5194/ADGEO-12-59-2007]
[7]  
[Anonymous], 2006, THESIS
[8]   Synoptic features associated with dust transition processes from North Africa to Asia [J].
Awad, Adel M. ;
Mashat, Abdul-Wahab S. .
ARABIAN JOURNAL OF GEOSCIENCES, 2014, 7 (06) :2451-2467
[9]   European cyclone track analysis based on ECMWF ERA-40 data sets [J].
Bartholy, Judit ;
Pongracz, Rita ;
Pattantyus-Abraham, Margit .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2006, 26 (11) :1517-1527
[10]   Climate predictability experiments with a general circulation model [J].
Bengtsson, L ;
Arpe, K ;
Roeckner, E ;
Schulzweida, U .
CLIMATE DYNAMICS, 1996, 12 (04) :261-278