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机构地区:[1]兰州城市学院,甘肃兰州730070 [2]中国科学院寒区旱区环境与工程研究所,甘肃兰州730000
出 处:《中国沙漠》2014年第2期542-549,共8页Journal of Desert Research
基 金:国家科技支撑计划项目(2011BAC07B02);国家自然科学基金项目(31300388;41361013);国家重点基础研究发展计划项目(2009CB421303)资助
摘 要:利用回归分析、小波分析和Mann-Kendall (M-K)突变分析研究了1970—2010年奈曼旗的降水变化特征。结果表明:(1) 不同雨量级中,0-5 mm降水事件最多,占全年降水事件的70%以上,其降水量也最多,占全年降水量的18%;降水间隔期以0-5 d为主,占全年无降水期的73%。(2) 1970—2010年奈曼旗年降水及季降水波动较大,基本呈相对少雨期和相对多雨期相间分布的特征;年降水及春、夏、秋和冬季降水的倾向率分别为-12.4、0.8、-3.2、-1.3 mm/10a和-0.3 mm/10a; 年降水及春、夏和秋季降水在1990年左右以正距平为主,而在1985年之前和1995年以后以负距平为主;冬季降水基本随年份增加呈减少的趋势。(3) 1月降水量最少,7月最多。7月降水量约占年降水量的30%以上,且与其他各月相比均有显著差异。(4) 通过小波分析发现,奈曼旗年降水存在6-8年的较短周期和17年左右的较长周期变化;年降水和夏、秋及冬季降水在进入21世纪后都有减少趋势。(5) M-K突变分析表明,奈曼旗年降水减少及春季降水增加的突变点分别为 2004年和2006年。The change trends of Naiman's precipitation patterns during 1970-2010 were analyzed by using linear regression, wavelet analysis and Mann-Kendall (M-K) mutation analysis. The results showed that, (1) Precipitation in the research area was dominated by small precipitation events with 0-5 mm, accounted for 70% of the total events, and up to 18% of the total precipitation amount. The precipitation interval was dominated by 0-5 days, accounted for 73% of the total days without precipitation. (2) In 1970-2010, the annual precipitation and seasonal precipitation changed complex, shown a dry wet dry process; The tendency rate of annual precipitation and spring, summer, autumn and winter precipitation was 12.4, 0.8, 3.2, 1.3 and 0.3 mm/10a, respectively; Annual precipitation and spring, summer and autumn precipitation have been positive anomaly about 1990, and negative anomaly before 1985 and after 1995. Winter precipitation showed a decreasing trend generally. (3) The precipitation was least in January, while a greatest in July and the July's precipitation accounted for more than 30% of the total precipitation amounts. And there was a significant difference in precipitation amount between the July and the other month. (4) Morlet wavelet analysis found that annual precipitation had a shorter cyclical fluctuation of 6-8 years and a longer cyclical fluctuation of 17 years in this region. Annual precipitation and summer, autumn and winter precipitation decreased in the beginning of the 21st century; (5) M-K mutation analysis showed that a reduce trend for annual precipitation and an increase trend for spring precipitation, and the start of abrupt time was 2004 and 2006, respectively.
关 键 词:科尔沁沙地 降水 小波分析 Mann-Kendall突变分析
分 类 号:P426.6[天文地球—大气科学及气象学]
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