首页|1961-2023年柴达木盆地降水日数时空分布特征

1961-2023年柴达木盆地降水日数时空分布特征

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根据柴达木盆地10个气象观测站点1961-2023年共63年的逐日降水量资料,应用气候倾向率法、Mann-Kendall法、Morlet小波变换和经验正交函数分解等气象统计分析方法,分析了柴达木盆地不同等级降水日数的时空分布;结果表明:(1)柴达木盆地年小雨、中雨、大雨日数的峰值出现在7月,暴雨日数峰值在8月,无大暴雨和特大暴雨发生.(2)柴达木盆地年小雨日数随时间变化表现出明显减少趋势;年中雨、大雨日数随时间变化表现出明显增加趋势.(3)柴达木盆地年小雨、中雨、大雨日数的突变年份分别为2011、1993、2007年.(4)年小雨日数主要周期为22 a;年中雨日数主要周期为10a;年大雨日数主要周期为20 a.(5)年小雨日数第一模态显示区域整体一致的特征,第二模态显示东西反相位的特征;年中雨日数第一模态显示东西反相位的特征,第二模态显示中东部多、两部少的特征;年大雨日数第一模态显示中东部多、两部少的特征,第二模态显示区域整体一致特征,第三模态显示东西反相位的特征.
Spatial and Temporal Distribution Characteristics of Precipitation Days in Qaidam Basin
Based on the daily precipitation data of 10 meteorological observation stations in Qaidam Basin for a total of 63 years from 1961 to 2023,the temporal and spatial distribution of precipitation days of different grades in Qaidam Basin was analyzed by meteorological statistical analysis methods such as climatic propensity rate method,Mann-Kendall method,Morlet wavelet transform and empirical orthogonal function(EOF)analysis.The results showed that:(1)The peak numbers of days of light,moderate and heavy rainfall in the Qaidam Basin occurred in July,and the peak number of days of rainstorm was in August.No extremely heavy rainstorms or catastrophic rainstorms had been recorded.(2)The annual number of days of light rainfall in the Qaidam Basin showed an obvious decreasing trend over time,while the annual number of days of medium and heavy rainfall showed a significant increasing trend.(3)The abrupt changes in the annual number of days of light rain,medium rain and heavy rain in the Qaidam Basin occurred in 2011,1993 and 2007,respectively.(4)The main periods of the annual number of days of light rain,moderate rain and heavy rain were 22 years,10 years and 20 years,respectively.(5)The first mode of the annual number of days of light rain showed a consistent spatial pattern across the region,while the second mode showed an east-west anti-phase pattern.For moderate rain,the first mode showed an east-west anti-phase feature,and the second mode showed the feature of more days in central-eastern region and fewer days in other regions.For heavy rain,the first mode indicated the pattern of more days in central-eastern region and fewer days in other regions,and the second mode showed a consistent feature across the region,while the third mode showed an east-west anti-phase feature.

Qaidam BasinClimatic propensity rateMorlet wavelet transformEmpirical orthogonal function

胡嘉玥、袁淑杰、苏丽欣、袁东升、施红霞

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成都信息工程大学大气科学学院,四川成都 610225

吉林省气象科学研究所,吉林长春 130062

长白山气象与气候变化吉林省重点实验室,吉林长春 130062

柴达木盆地 气候倾向率 Morlet小波变换 经验正交函数分解

2024

内蒙古气象
内蒙古气象局 内蒙古气象气象学会

内蒙古气象

影响因子:0.206
ISSN:1005-8656
年,卷(期):2024.(5)