Using the SPI to interpret spatial and temporal conditions of drought in China

被引:4
作者
Wagan, Bakhtawar [1 ,2 ]
Zhang, Zhanyu [1 ]
Feng Baopeing [1 ]
Wagan, Hakimzadi [3 ]
Han, Si [1 ]
Ahmad, Ijaz [1 ]
Kabo-Bah, Amos T. [4 ]
机构
[1] Hohai Univ, Coll Water Conservancy & HydroPower Engn, Nanjing 210098, Jiangsu, Peoples R China
[2] Sind Agr Univ, Dept Farm Struct, Fac Agr Engn, Tandojam, Pakistan
[3] Isra Univ, Dept Management Sci, Fac Commerce Econ & Management Sci, Hyderabad 71000, Sindh, Pakistan
[4] Univ Energy & Nat Resources, Dept Energy & Environm Engn, Sunyani, Ghana
关键词
drought; drought index; precipitation; Zhanghe River Basin; STANDARDIZED PRECIPITATION INDEX; RAINFALL; TRENDS; REGIONS;
D O I
10.5367/oa.2015.0217
中图分类号
S [农业科学];
学科分类号
09 ;
摘要
The start and duration of a drought are often not easy to define. The advance and onset are usually slow and the social and economic impacts can then extend over a long period. In this study, the Standardized Precipitation Index (SPI) was used to describe and compare droughts in different periods and regions under different climatic conditions. The importance of the index lies in its simplicity and in its ability to identify the beginning and end of a drought event. Thus it may be a useful tool for drought contingency planning. This paper examines the SPI by evaluating its application using historical precipitation data from nine weather stations in China. Different time series data covering the period 1980 to 2011 and for differing timescales of 3, 9 and 24 months were used. The results underline the potential of the SPI to inform drought alerts and forecasting efforts as part of a drought contingency planning strategy.
引用
收藏
页码:235 / 241
页数:7
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