马玉坤, 马俊强, 李菲, 马旭洁. 青藏高原边坡临夏地区短时强降水时空分布及海拔特征分析[J]. 沙漠与绿洲气象, 2022, 16(3): 68-74.
引用本文: 马玉坤, 马俊强, 李菲, 马旭洁. 青藏高原边坡临夏地区短时强降水时空分布及海拔特征分析[J]. 沙漠与绿洲气象, 2022, 16(3): 68-74.
MA Yukun, MA Junqiang, LI Fei, MA Xujie. Spatial and Temporal Characteristics of Short-time Strong Rainfall and Its Altitude Distrbution Characteristics in Linxia at Plateau Slope[J]. Desert and Oasis Meteorology, 2022, 16(3): 68-74.
Citation: MA Yukun, MA Junqiang, LI Fei, MA Xujie. Spatial and Temporal Characteristics of Short-time Strong Rainfall and Its Altitude Distrbution Characteristics in Linxia at Plateau Slope[J]. Desert and Oasis Meteorology, 2022, 16(3): 68-74.

青藏高原边坡临夏地区短时强降水时空分布及海拔特征分析

Spatial and Temporal Characteristics of Short-time Strong Rainfall and Its Altitude Distrbution Characteristics in Linxia at Plateau Slope

  • 摘要: 利用青藏高原边坡临夏地区6个国家级自动气象站和66个乡镇区域自动气象站2010—2019年5—9月逐小时降水资料,分析了临夏地区短时强降水的时空分布及海拔、地形特征,结果表明:近10 a短时强降水频次总体呈上升趋势,短时强降水频次与西太平洋副热带高压脊线位置和北界位置有密切关系。短时强降水主要发生在5—9月,集中时段为7月中旬—8月中旬,19—23时为高发时段,属于傍晚型和夜雨型。近10 a临夏地区短时强降水的极端性逐年增大,单站年均频次在0.2~2.6次,平均为0.8次,短时强降水空间分布差异较大,总体呈西南多、东部和北部少,山区多、川区少的特征。临夏地区降水分布与海拔高度有明显关系,5—9月平均降水量随海拔高度升高而增大,不同海拔、地形下短时强降水频次分布呈现两个极端:海拔较高的山地喇叭口地形区域和海拔较低的河谷地区,是临夏地区汛期短时强降水的重点关注区域。

     

    Abstract: Based on hourly precipitation data at 6 national automatic weather stations and 66 township regional automatic weather stations from May to September during 2010-2019,the spatial and temporal distribution characteristics of short-time heavy rainfall were discussed in detail,combined with influences of altitude and plateau slope topography on short-time heavy rainfall in Linxia area on plateau slope.The frequency presented an upward trend in recent 10 years,and it was related to the location of the ridge line and the northern boundary of the western Pacific subtropical high.The shorttime heavy rainfall mainly occurred from May to September,the concentrated period was from mid-July to mid-August.The high frequency period of heavy rain was from 19:00 to 23:00,belonging to the evening and the night rain type.The extremeness increased in recent 10 years.The average annual frequency of a single station was between 0.2 and 2.6,with an average of 0.8 times. The spatial distribution of short-term heavy rainfall was quite different,which was generally characterized by“higher in the southwest and lower in the northeast,higher in mountainous areas and lower in valley areas”.The precipitation distribution showed a significant relationship with altitude:the average precipitation from May to September increased with the altitude.The frequency distribution of short-term heavy rainfall showed two extremes:the mountainous trumpet terrain area with higher altitude and the valley area with lower altitude,which were the key areas for short-term heavy rainfall in flood season in Linxia area.

     

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