| 甘肃省黄土高原区夏季极端降水的时空特征 |
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| 引用本文： | 王兴梅,张勃,戴声佩,张凯,马中华,王亚敏.甘肃省黄土高原区夏季极端降水的时空特征[J].中国沙漠,2011,31(1):223-229. |
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| 作者姓名： | 王兴梅 张勃 戴声佩 张凯 马中华 王亚敏 |
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| 作者单位： | 1. 西北师范大学,地理与环境科学学院,甘肃,兰州,730070
2. 中国气象局兰州干旱气象研究所,甘肃省干旱气候变化与减灾重点实验室/中国气象局干旱气候变化与减灾重点开放实验室,甘肃,兰州,730020 |
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| 基金项目： | 国家自然科学基金，公益性行业(气象)科研专项，中国科学院知识创新工程重要方向项目，甘肃省自然科学基金，生态经济学甘肃省级重点学科 |
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| 摘 要： | 借助ArcGIS和Matlab数据软件平台,运用复值Morlet小波分析和数理统计方法对甘肃省黄土高原区夏季极端降水的频数和强度在时空上的变化特征进行分析。结果表明:①近半个世纪以来,该区极端降水事件发生的频数和强度在6、7月周期较长,8月周期较短:即6、7月极端降水事件发生的主周期是11~12 a,8月是4~5 a的周期。②从空间尺度来看,该区夏季极端降水带移动由西向东表现为:大致以庄浪、秦安、天水一线为界,6月频数和强度大值区在这一线以西海拔相对高的山区,而7—8月在这一线以东地区,尤其是陇东地区的东南部。③总体趋势是6月极端降水频数和强度明显呈上升趋势;7月极端降水频数和强度呈下降趋势;8月极端降水频数呈下降趋势,强度呈微弱上升趋势。
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| 关 键 词： | 极端降水 小波分析 时空特征 黄土高原 |
| 收稿时间： | 2010-1-25 |
| 修稿时间： | 2010-3-12 |
Spatial and Temporal Characteristics of Summer Extreme Precipitation in Loess Plateau of Gansu Province,China |
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| WANG Xing-mei,ZHANG Bo,DAI Sheng-pei,ZHANG Kai,MA Zhong-hua,WANG Ya-min.Spatial and Temporal Characteristics of Summer Extreme Precipitation in Loess Plateau of Gansu Province,China[J].Journal of Desert Research,2011,31(1):223-229. |
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| Authors: | WANG Xing-mei ZHANG Bo DAI Sheng-pei ZHANG Kai MA Zhong-hua WANG Ya-min |
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| Institution: | WANG Xing-mei1,ZHANG Bo1,DAI Sheng-pei1,ZHANG Kai2,MA Zhong-hua1,WANG Ya-min1(1.School of Geography and Environment Science,Northwest Normal University,Lanzhou 730070,China,2.Key laboratory of Arid Climatic Change and Disaster Reduction of Gansu Province/Key Open Laboratory of Arid Climatic Change and Disaster Reduction of CMA,Institute of Arid Meteorology,China Meteorological Administration,Lanzhou 730020,China) |
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| Abstract: | Based on ArcGIS and Matlab software platform, the spatial and temporal characters of frequency and intensity of summer extreme precipitation in 1961—2009 in Loess Plateau of Gansu Province, China are investigated by use of complex Morlet wavelet analysis and mathematical statistics. Following conclusions are concluded. (1)Variation of frequency and intensity of summer extreme precipitation has a longer fluctuation period in June and July than in August, and the main period in June and July is 11—12 a, but the main period in August is 4—5 a.（2）Summer extreme precipitation zone in Loess Plateau of Gansu Province transfers from west to east. The line from Zhuanglang-Qinan-Tianshui is its eastern boundary. The extreme precipitation zone in June is in the western high mountainous area, and the zone in July and August is in the eastern area, particularly in the south-eastern part of Longdong region.（3）The overall trend of the frequency and intensity of extreme precipitation in June is a upward trend, and the trend in July is downward. In August, the trend of extreme precipitation frequency is downward, but the intensity shows a slight upward trend. |
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| Keywords: | extreme precipitation Morlet wavelet analysis spatial and temporal characteristics Loess Plateau |
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