中国农业气象 ›› 2010, Vol. 31 ›› Issue (S1): 10-15.

• 论文 • 上一篇    下一篇

洱海流域近59年水资源的多时间尺度分析

李文娟;严昌荣;刘恩科;彭正萍;刘勤;   

  1. 河北农业大学资源与环境科学学院;中国农业科学院农业环境与可持续发展研究所/农业部旱作节水农业重点开放实验室;
  • 出版日期:2010-12-20 发布日期:2010-12-20
  • 基金资助:

    国家水体污染控制与治理科技重大专项(2008ZX07105-002-04);; GEF项目“农业综合开发适应气候变化”课题;; 中央级公益性科研院所基本科研业务费专项资助课题“洱海流域农业水管理与水分生产力评价”

Multiple Time Scale Analysis of Water Resources in Erhai Lake Basin in Recent 59 Years

LI Wen-Juan1,YAN Chang-Rong2,LIU En-ke2,PENG Zheng-ping1,LIU Qin2(1.College of Resources and Environmental Sciences,Agricultural University of Hebei,Baoding 071001,China;2.Institute of Environment and Sustainable Development in Agriculture,CAAS/Key Laboratory of Dryland Agriculture,MOA,Beijing 100081)   

  • Online:2010-12-20 Published:2010-12-20

摘要: 以分析洱海流域地区水资源的时序变化特征为研究目标,利用国家气象局整编的大理气象站气象资料(1951-2009年),用FAO推荐的Penman-Monteith公式计算潜在蒸散量,分析了近59a来洱海流域地区降水和蒸散量的变化特征,并分析计算了相应的降蒸差及其演变特征。结果表明:(1)各年代降水量呈现了一个先减少后增加的变化规律,春季降水量有显著上升趋势,线性倾向值为13.6mm/10a,夏季各年代降水量呈现了一个先减后增加的变化规律,秋季降水量大体经历了"少-多-少"的变化过程,年降水量发生的两次突变都是由少雨期到多雨期,春季、夏季和冬季降水发生了明显的突变,春季和冬季突变后进入多雨期,而夏季进入少雨期;(2)年蒸散量在波动中有减少的趋势,达到7.8mm/10a,春季、夏季和冬季的蒸散量呈现波动变化特点,最近10a呈现显著减少的趋势,秋季的蒸散量呈现显著的减少趋势,达3.0mm/10a。年蒸散量和春季蒸散量存在明显的突变现象,但不是在同一时期发生,目前都处于低蒸散期;(3)年内降水量和降蒸差的逐月变化趋势基本相同,但月间分布不均衡,蒸散量逐月变化趋势呈现5月为最大值的近似单峰抛物线的线型分布;(4)未来本地区冬、春、秋季节干旱依然存在,影响作物尤其是坡耕地玉米和冬季大蒜的正常生长和发育。

关键词: 降水, 蒸散, 降蒸差, 突变分析

Abstract: Climate change is acknowledged as one of the most critical problem that human being has ever been faced,which has a complex impact on water resource.With the overwhelming emphasis on developing the time series variation characteristics of water resource,based on the meteorological data of meteorological administration from 1951 to 2009,this paper estimated potential evapotranspiration(E) and difference of precipitation and evaporation(W) by the Penman-Monteith model of Food and Agriculture Organization(FAO) nominated in 1998 and analyzed evolution characteristics of precipitation(P),E and W in Erhai Lake Basin.The result showed that annual precipitation varied in different decades with a decreased and then increased trend in the recent 59 years.Meanwhile,annual spring precipitation varied in different years with an increased trend,with a linear trend value of 13.6 mm per 10 years.Annual summer precipitation had a same trend in different decades.Moreover,autumn precipitation had a "less-more-less" trend in general.The result of Mann-Kendall analysis indicated that the mainly two time point mutation were 1995 and 2005,in which year annual precipitation showed a mutation from less to more in Erhai Lake Basin.Meanwhile,spring,summer and winter precipitation showed a remarkable mutation,not as in autumn.The result also showed that annual and autumn evaporation varied in different years with a decreased trend in the recent 59 years,with a linear trend value of 6.8 mm per 10 years and 3.0 mm per 10 years respectively.In addition,the evaporation of three other seasons had a fluctuation change and varied with a significant decreased trend in last several years.The evaporation of Mann-Kendall analysis indicated that the mutation occurred in different years and that the period of less evaporation continued in last several years.The seasonal distribution of precipitation,and available water resources was not in accordance with the monthly distribution.Simultaneously,the seasonal distribution of evaporation showed an approximate parabola with a max value in May.The risks of the future droughts for spring,autumn and winter in this region still existed,which will restrict the development of garlic for winter and corn in slop land.

Key words: Precipitation, Evapotranspiration, Difference of precipitation and evapotranspiration, Mutation analysis