globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6403606
论文题名:
峨眉山及其周边地区降水气候特征研究
其他题名: Study on the Climate Characteristics of Precipitation in Emei Mountain and Its Surrounding Area
作者: 吕晶1; 李忠贤2; 李跃清3; 邹槟骏4; 江南4; 李雪枫4
刊名: 高原气象
ISSN: 1000-0534
出版年: 2018
卷: 37, 期:6, 页码:571-579
语种: 中文
中文关键词: 峨眉山 ; 降水量 ; 雨日 ; 降水频次 ; 区域气候变化
英文关键词: Emei Mountain ; amount of precipitation ; rain day ; precipitation frequency ; regional climate change
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 基于1959-2016年峨眉山、峨眉市、乐山市及夹江县气象站逐日降水数据和1964-2016年6-9月逐时降水数据,应用统计诊断分析方法,研究了峨眉山及其周边地区降水量、雨日和降水频次的多时间尺度变化特征。结果表明,峨眉山及其周边地区年代降水变化趋势基本一致,但随海拔具有一定差异性,高海拔峨眉山趋势更明显。峨眉山与其周边地区年降水量和年雨日均在20世纪90年代后显著减少,且峨眉山年雨日比其周边地区减少更快。汛期峨眉山及其周边地区降水量、雨日变化均强于其年代和年降水量、雨日变化,较其他时段更突出;高海拔峨眉山冬季、秋季和夏季降水量减少趋势显著,而周边地区夏季和秋季降水量减少趋势明显;峨眉山及其周边地区四季雨日都呈减少趋势,但峨眉山减少程度大于其周边地区。峨眉山及其周边地区月降水量和雨日都呈减少趋势,但峨眉山更明显。峨眉山降水量日变化呈单峰单谷结构,而峨眉市则在清晨出现次峰值,两地夜雨特征突出,夜间降水量远大于白天,且两地降水量峰值出现时间都存在提前的变化特征;峨眉山小时降水频次最大值出现时间存在提前的变化特征,但峨眉市相反,具有延后的变化特征。在全球气候变暖下,峨眉山及其周边地区气候响应主要为降水减少,高海拔地区降水减少的趋势大于低海拔地区。峨眉山及其周边地区这种区域气候响应的一致性与差异性,可能与区域温度响应与水汽状况差异有关。
英文摘要: Based on the daily precipitation data of Emei Mountain,Emei City,Leshan City and Jiajiang County meteorological stations from 1959 to 2016 and their hourly precipitation data during June-September from 1964 to 2016,the multiple time scale variation characteristics of the amount of precipitation,rain days and precipitation frequency in Emei Mountain and its surrounding area were studied by statistical analysis and diagnosis methods. The result shows that the decadal precipitation and rain days decrease in Emei Mountain and its surrounding area in the past few decades,and the decrease degree of high-altitude Emei Mountain is stronger than that of low-altitude surrounding area. The annual precipitation and annual rain days decrease significantly in Emei Mountain and its surrounding area after the 1990s,and the annual rain days in Emei Mountain decreases faster. In flood season, the variations of amount of precipitation and rain days in Emei Mountain and its surrounding area are stronger than their interdecadal and interannual variations,and it is more prominent than the other periods. Except in spring,the precipitation in high-altitude Emei Mountain in other three seasons reduces significantly,and it obviously reduces in summer and autumn in low-altitude surrounding area. The decrease of rain days in all seasons is more obvious in Emei Mountain than in its surrounding area. The reduction of monthly precipitation and rain days in Emei Mountain is more obvious that that in its surrounding area. The diurnal variation of precipitation in highaltitude Emei Mountain has single-peaked and single-valley distribution,but the second peak appears in the morning in low-altitude Emei City. The precipitation of Emei Mountain and its surrounding area is much larger in the night than that in the daytime. The peak time of precipitation in Emei Mountain and Emei City occurs earlier than before. The time of maximum hourly precipitation frequency has significantly advancing feature in Emei Mountain. But Emei City has the variation of being delayed. Under the global warming,the precipitation in Emei Mountain and its surrounding area significantly decreases,especially in Emei Mountain. The consistency and difference of regional climate response in Emei Mountain and its surrounding area may be related to regional temperature responses and water vapor conditions.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/154165
Appears in Collections:气候变化事实与影响

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作者单位: 1.南京信息工程大学
2.乐山市气象局, 气象灾害教育部重点实验室
3.气候与环境变化国际联合实验室
4.气象灾害预报预警与评估协同创新中心
5., 南京
6.乐山, 江苏
7.四川 210044
8.614000, 中国
9.南京信息工程大学, 气象灾害教育部重点实验室
10.气候与环境变化国际联合实验室
11.气象灾害预报预警与评估协同创新中心, 南京, 江苏 210044, 中国
12.中国气象局成都高原气象研究所, 成都, 四川 610072, 中国
13.乐山市气象局, 乐山, 四川 614000, 中国

Recommended Citation:
吕晶,李忠贤,李跃清,等. 峨眉山及其周边地区降水气候特征研究[J]. 高原气象,2018-01-01,37(6):571-579
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