马拉维降雨时间序列波动:对选定地区的分析

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geofizika Pub Date : 2014-06-30 DOI:10.15233/GFZ.2014.31.1
Chisomo Patrick Kumbuyo, H. Yasuda, Y. Kitamura, K. Shimizu
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引用次数: 38

摘要

利用选定雨量站的31年时间序列研究了马拉维降雨的年际波动,目的是分析马拉维降雨的时空特征。研究发现降水量年际波动较大,地形和地理位置对年降水量分布起主要作用。季节指数和降水集中指数表明,降水具有强季节性和高度集中性,除恩哈塔贝站为季节性降水外,其余站均为3个月降水。年内降水分布具有很大的时空变异性。站间的相互关系表明两个明显的区域,第1区由Karonga和Nkhatabay组成,第2区由Bolero、Kasungu、Salima、Dedza、Mangochi、Makoka和Ngabu组成。降雨时间序列的光谱分析显示周期为5至8年,表明与厄尔尼诺南方涛动有关,并且是准两年一次涛动周期的两倍。除了共同的周期外,两个区降水时间序列的周期分别为13.64年和10.06年,与太阳周期有关。这些周期与在其他南部非洲国家发现的周期一致。
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Fluctuation of rainfall time series in Malawi: An analysis of selected areas
Inter annual fluctuation of rainfall in Malawi was studied using a 31 year time series from selected rain gauge stations with the aim of analyzing the spatial and temporal characteristics of rainfall in Malawi. The study found strong inter-annual fluctuation of rainfall, with topography and location playing major roles in the annual rainfall distribution. The seasonal index and precipitation concentration index showed that rainfall is highly seasonal and highly concentrated with most stations receiving rainfall in three months, except for Nkhatabay which has seasonal rainfall. The intra annual rainfall distribution was highly variable in time and space. Cross correlations among the stations suggested two distinct zones, zone 1 composed of Karonga and Nkhatabay and zone 2 composed of Bolero, Kasungu, Salima, Dedza, Mangochi, Makoka and Ngabu. Spectral analysis of the rainfall time series revealed cycles at five to eight years, suggesting links with the El Nino Southern Oscillation and double the period of the Quasi Biennial Oscillation. Apart from the common cycles, the rainfall time series of the two zones showed periods of 13.64 and 10.06 years, respectively, which suggests links with the solar cycle. These cycles are consistent with those found in other southern Africa countries.
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来源期刊
Geofizika
Geofizika 地学-地球化学与地球物理
CiteScore
1.60
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: The Geofizika journal succeeds the Papers series (Radovi), which has been published since 1923 at the Geophysical Institute in Zagreb (current the Department of Geophysics, Faculty of Science, University of Zagreb). Geofizika publishes contributions dealing with physics of the atmosphere, the sea and the Earth''s interior.
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