摘要
以干旱高发区贵州省为研究对象,利用贵州省19个站点1960—2013年气象日值资料,考虑气象干旱累积效应及当地秋收农作物生长时期需水要求,验证了秋收作物生育期内标准降水蒸散指数(Sep-SPEI-6)与粮食减产量之间的相关性。基于Sep-SPEI-6指数采用MannKendall法、滑动t检验、Morlet小波周期分析以及Hurst指数等方法分析了贵州省干旱时空变化特征。结果表明:1 Sep-SPEI-6与贵州省及各州、市粮食减产量呈极显著负相关性。2在1991、2001年前后贵州省气候发生了突变。3与第一阶段(1960—1991年)相比,第二阶段(1992—2001年)干旱发生频率和影响范围均减少了10.59%;较第二阶段,第三阶段(2002—2013年)分别增加了23.67%和24.74%;与前两阶段相比,第三阶段的干旱历时与强度增加显著。4 Sep-SPEI-6时间序列存在明显的周期性振荡特征,以22 a为第1主周期。5各站点Sep-SPEI-6的Hurst数值均大于0.5,说明其变化具有较好的持续性。6干旱易发区呈现由东向西的转移趋势。7农作物生长期内日降水>1 mm天数和日照总时数是影响农作物生长期干旱的主要气象因素。研究成果为贵州省抗旱减灾措施的制定提供了理论依据。
Guizhou is an important agriculture area locating in the southwest of China with maize and rice as its main food crops. Food security here is of great importance to maintain the stability of the minorities. However, droughts have frequently taken place recently, and resulted in big reductions in the crop yield. Under the circumstance of global climate change, therefore,the understanding of the temporal and spatial characteristics of drought and its relation with the climate mutation is of necessity for drought prevention and mitigation. We collected the daily meteorological data of 19 stations in Guizhou Province during 1960-2013. In consideration of the accumulated drought effect and the water requirement of autumn crops, the standard Precipitation- Evaporation index at six- month time scale between April and September(SepSPEI- 6) was calculated. The correlation analysis between Sep- SPEI- 6 and the crop yield reduction was tested. By use of multiple methods, i.e., Mann- Kendall, sliding t- test, Morlet wavelet cycle analysis and Hurst index, the spatial and temporal variation of drought were analyzed. Some results were obtained as bellow. Sep- SPEI- 6 in Guizhou Province and the 9cities showed a significant negative correlation with the annual crop yield reduction. The climate mutation occurred twice around year 1991 and year 2001. Compared with that in the first phase between 1960 and 1991, the occurring frequency and extent of droughts in the second stage between 1992 and 2001 decreased 10.59%. Compared with that in the second stage, the occurring frequency and extent of droughts increased 23.67% and 24.74%respectively in the third phase between 2002 and 2013. In contrast to the former two stages, the third one had significantly increased duration and intensity of drought. There was an obvious periodic oscillation in time series of Sep-SPEI-6, and 22 years was the first primary period. The Hurst index of Sep- SPEI- 6 at different stations were all greater than 0.5, suggesting a better continuity in the Sep- S
出处
《自然资源学报》
CSSCI
CSCD
北大核心
2015年第10期1735-1749,共15页
Journal of Natural Resources
基金
水利部公益性行业科研专项(201301039)
贵州省水利厅科技专项经费项目(KT201313)
国家自然科学基金项目(41271236)
河南省科技攻关计划项目(142102110058
142102310290)
华北水利水电大学青年科技创新人才项目(70459)
华北水利水电大学创新计划项目(HSCX2004059)
