%0 Journal Article
%T 吉林省四平地区近50年区域旱涝变化特征<br>Variation of drought and flood frequency in Siping region in the past 50 years
%A 郑蕾
%A 王佳楠
%A 魏婷婷
%A 刘爽
%J 干旱地区农业研究
%D 2017
%R 10.7606/j.issn.1000-7601.2017.04.43
%X 应用国家气候中心下发的吉林省四平市5站的逐日降水资料对四平市进行旱涝等级划分，主要应用线性趋势法和小波分析法对其特征进行分析，根据旱涝指标Z指数对旱涝指数W指数进行运算。结果分析得出：W指数存在较弱的下降趋势，并且阶段性特征变化明显，W指数计算得出严重旱年与降水距平百分率有很好的对应关系；54年四季旱涝年数差异较大，各季存在旱涝交替、连旱或连涝的特征；年W指数以3.68·10a-1的速度递减，春季和冬季W旱涝指数以3.89·10a-1和10.183·10a-1的速率增加，均通过0.05水平的显著性检验，呈现增加趋势，夏季和秋季W旱涝指数呈现递减趋势。从小波分析结果得出各季节震荡周期不同并且特征显著。<br>Based on the calculation of the drought-flood index (Z index, W index) with the daily precipitation data of 5 meterological stations, the variation of drought-flood in Siping region was analyzed by the linear trend method and wavelet analysis method. The results showed that the W index data was in a weak downward trend in the Siping during the past 54 years, and exhibited alternating drought and flooding. The extreme drought year of W index corresponded to the precipitation anomaly year. These two had consistency and W index might well reflect the flood/drought rules of Siping region. The drought parameter W tends to decreased at a rate of 3.68·10a-1, while it tends to increased significantly at the rate of 3.89·10a-1 in spring, and 10.183·10a-1 in winter. Each season has a different oscillation period and distinguished feature according to the result of the wavelet analysis method.
%K 四平地区 旱涝变化 W指数 小波分析法&lt
%K br&gt
%K Siping region flood and drought frequency W index wavelet analysis method
%U http://ghdqnyyj.ijournal.cn/ghdqnyyj/ch/reader/view_abstract.aspx?file_no=20170443&flag=1