Variability of seasonal and annual precipitation in Slovenia and its correlation with large-scale atmospheric circulation

被引:21
作者
Milosevic, Dragan D. [1 ]
Savic, Stevan M. [1 ]
Pantelic, Milana [1 ]
Stankov, Ugljesa [2 ]
Ziberna, Igor [3 ]
Dolinaj, Dragan [1 ]
Lescesen, Igor [4 ]
机构
[1] Univ Novi Sad, Climatol & Hydrol Res Ctr, Fac Sci, Trg Dositeja Obradovica 3, Novi Sad 21000, Serbia
[2] Univ Novi Sad, Ctr Spatial Informat Vojvodina Prov, Fac Sci, Trg Dositeja Obradovia 3, Novi Sad 21000, Serbia
[3] Univ Maribor, Fac Arts, Dept Geog, Koroska Cesta 160, Maribor, Slovenia
[4] Univ Novi Sad, Dept Geog Tourism & Hotel Management, Fac Sci, Trg Dositeja Obradovica 3, Novi Sad 21000, Serbia
关键词
precipitation; atmospheric circulation; North Atlantic Oscillation; Mediterranean Oscillation; Western Mediterranean Oscillation; Slovenia; NORTH-ATLANTIC OSCILLATION; CLIMATE VARIABILITY; RAINFALL TRENDS; PATTERNS; TELECONNECTION; PRESSURE; REGION; TEMPERATURES; PROJECTIONS; MOISTURE;
D O I
10.1515/geo-2016-0041
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This paper examines temporal and spatial variability and trends of annual and seasonal precipitation in Slovenia and their relationship with three atmospheric circulation patterns represented by their indices: North Atlantic Oscillation index (NAOi), Mediterranean Oscillation index (MOi) and Western Mediterranean Oscillation index (WeMOi). Data from 45 precipitation stations were used for the period 1963-2012. Mean annual precipitation varies from 736 mm in eastern Slovenia to 2,518 mm in northwestern Slovenia. A significant annual precipitation decrease (from -3% to -6% per decade) is observed in western Slovenia. Significant negative trends are observed in southwestern Slovenia in summer (from -4% to -10% per decade) and near the Adriatic coast in spring (from -6% to -10% per decade). Non-significant negative and positive trends are observed in winter and autumn, respectively. Results indicate significant correlations between winter precipitation and MOi (from -0.3 to -0.7), NAOi (from -0.3 to -0.6) and WeMOi (from 0.3 to 0.6). Significant WeMOi influence is observed in spring and autumn, while NAOi and MOi influence has not been detected. Annual precipitation and WeMOi are significantly correlated in central and eastern Slovenia, while significant NAOi and MOi influence is observed in western Slovenia (with the larger area covered by MOi influence).
引用
收藏
页码:593 / 605
页数:13
相关论文
共 56 条
[1]  
ADAMIC M. OROZEN, 2004, SLOVENIA GEOGRAPHICA, P7
[2]   A HOMOGENEITY TEST APPLIED TO PRECIPITATION DATA [J].
ALEXANDERSSON, H .
JOURNAL OF CLIMATOLOGY, 1986, 6 (06) :661-675
[3]   Do atmospheric teleconnection patterns influence rainfall erosivity? A study of NAO, MO and WeMO in NE Spain, 1955-2006 [J].
Angulo-Martinez, Marta ;
Begueria, Santiago .
JOURNAL OF HYDROLOGY, 2012, 450 :168-179
[4]  
[Anonymous], 2002, DETECTING TRENDS ANN
[5]   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
[6]   Analyzing the genesis, intensity, and tracks of western Mediterranean cyclones [J].
Bartholy, Judit ;
Pongracz, Rita ;
Pattantyus-Abraham, Margit .
THEORETICAL AND APPLIED CLIMATOLOGY, 2009, 96 (1-2) :133-144
[7]   Mountain climates and climatic change: An overview of processes focusing on the European Alps [J].
Beniston, M .
PURE AND APPLIED GEOPHYSICS, 2005, 162 (8-9) :1587-1606
[8]   Shifts in the distributions of pressure, temperature and moisture and changes in the typical weather patterns in the Alpine region in response to the behavior of the North Atlantic Oscillation [J].
Beniston, M ;
Jungo, P .
THEORETICAL AND APPLIED CLIMATOLOGY, 2002, 71 (1-2) :29-42
[9]  
Bergant K., STUDIA FORESTALIA SL, V130, P67
[10]   The North Atlantic Oscillation signal in a regional climate simulation for the European region [J].
Bojariu, R ;
Giorgi, F .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2005, 57 (04) :641-653