热带地理 ›› 2020, Vol. 40 ›› Issue (6): 1063-1074.doi: 10.13284/j.cnki.rddl.003293
董满宇1,2(), 田相佑2, 胡木兰2, 王磊鑫2, 江源1,2, 徐霞1,2
收稿日期:
2020-05-08
修回日期:
2020-09-02
出版日期:
2020-11-30
发布日期:
2020-12-10
作者简介:
董满宇(1983—),男,辽宁兴城人,博士,副教授,主要从事资源生态与区域气候研究,(E-mail)基金资助:
Received:
2020-05-08
Revised:
2020-09-02
Online:
2020-11-30
Published:
2020-12-10
摘要:
基于太湖流域1960—2017年逐日降水数据,运用Mann-Kendall非参数检验法、R/S分析等方法,分析太湖流域不同等级降水的时空变化特征,并探讨了不同等级降水对年降水的影响。结果表明:1)近60年来,流域小雨发生率最高,为73.55%;年总降水量中,中雨量所占比例最大,为32.05%。小雨发生率呈显著减少趋势,暴雨贡献率呈显著增加趋势。2)太湖流域大雨、暴雨的降水量和降水日数都呈显著增加,小雨日数显著减少,小雨强度、年总降水强度显著增强。3)不同等级降水变化趋势的空间分布存在明显差异。小雨日数与年总降水日数,以及小雨强度与年总降水强度的变化趋势空间格局相一致。中雨日数、大雨日数、暴雨日数变化趋势的空间分布与其对应的降水量变化趋势的空间格局相似。4)R/S分析结果显示,小雨、暴雨、年总降水相关指标(小雨量除外)都表现出较强的持续性,未来变化趋势与过去相一致。5)近60年来,太湖流域年总降水量、降水日数、年总降水强度的变化,分别受中雨量、小雨日数、暴雨量的影响较大。在旱年流域年降水量偏少受大雨量减少的影响较大,而涝年年降水量偏多受暴雨增加的影响较大。
中图分类号:
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