Characteristics of Summer Precipitation in Chongqing Based on Hourly Rain Gauges Data

IF 2.1 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Yi Liu, Yaping Zhang, Jianping Zhang, Yonghua Li, Danhua Zhai, Fang Luo, Yong Zhang, Guo-xing Zhou
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引用次数: 1

Abstract

Based on the hourly precipitation data of 34 meteorological stations in Chongqing in the summers (June to August) from 1996 to 2015, the spatial distribution and daily variation of precipitation amount (PA), precipitation intensity (PI), precipitation frequency (PF), and precipitation extremes in Chongqing are analyzed. The results show that, from the perspective of spatial distribution, the precipitation amount (PA) in Chongqing presents a distribution pattern of more around and less in the middle; the area with high precipitation intensity (PI) is mainly located in the northeast of Chongqing; the large value centers of precipitation frequency (PF) are located in the south and west of Chongqing and near Chengkou. On the spatial distribution of hourly precipitation, the precipitation in most areas of Chongqing is mainly concentrated at night [0200–0900 BT (1800–0100 UTC)], and the rain belt spreads from west to east with the passage of time. On the whole, interannual evolution characteristics of summer precipitation amount, precipitation intensity, and precipitation frequency in Chongqing are basically the same, showing a fluctuation characteristic without obvious trend, but there are some peaks and valleys. From the perspective of diurnal cycle, a larger peak of PA in Chongqing appears near 0300 BT (1900 UTC), another lower peak around 1200 BT (0400 UTC), a larger peak of PI around 0300 BT (1900 UTC), another smaller peak around 1500 BT (0700 UTC), and only one peak of PF around 0700 BT (2300 UTC). The extreme precipitation of different duration in summer in Chongqing is closely related to the topographic characteristics and weather system, the extreme centers of each diachronic precipitation are mainly located near Shapingba, Kaizhou, Youyang, and Shizhu, and the time evolution characteristics of the extreme precipitation are not obvious, but the trend of the extreme precipitation accumulated in 1 h, 3 h, 6 h, or 12 h is basically the same.
基于逐时雨量计的重庆市夏季降水特征
利用重庆市34个气象站1996~2015年夏季(6~8月)的小时降水资料,分析了重庆市降水量(PA)、降水强度(PI)、降水频率(PF)和极端降水的空间分布和日变化规律。结果表明,从空间分布的角度看,重庆市降水量呈现出周边多、中部少的分布格局;强降水区主要分布在重庆东北部;降水频率大值中心位于重庆市南部、西部、城口附近。在小时降水量的空间分布上,重庆大部分地区的降水主要集中在夜间[0200–0900 BT(1800–0100 UTC)],随着时间的推移,雨带由西向东扩展。总体而言,重庆夏季降水量、降水强度和降水频率的年际演变特征基本相同,呈现波动特征,没有明显的趋势,但也存在一些波峰和波谷。从日周期来看,重庆PA的一个较大峰值出现在0300 BT(1900 UTC)附近,另一个较低峰值出现在1200 BT(0400 UTC)左右,PI的一个较大峰值出现在10300 BT(1900UTC)附近;另一个较小峰值出现在1500 BT(0700 UTC)附近。PF只有一个峰值出现在0700 BT(2300 UTC)左右。重庆夏季不同持续时间的极端降水与地形特征和天气系统密切相关,各历时性降水的极端中心主要位于沙坪坝、开州、酉阳、石竹附近,极端降水的时间演化特征不明显,但1 h、 3 h、 6 h、 或12 h基本相同。
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来源期刊
Advances in Meteorology
Advances in Meteorology 地学天文-气象与大气科学
CiteScore
5.30
自引率
3.40%
发文量
80
审稿时长
>12 weeks
期刊介绍: Advances in Meteorology is a peer-reviewed, Open Access journal that publishes original research articles as well as review articles in all areas of meteorology and climatology. Topics covered include, but are not limited to, forecasting techniques and applications, meteorological modeling, data analysis, atmospheric chemistry and physics, climate change, satellite meteorology, marine meteorology, and forest meteorology.
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