Warm-Season Diurnal Variations of Total, Stratiform, Convective, and Extreme Hourly Precipitation over Central and Eastern China

• Published in: Advances in atmospheric sciences 2019-02, Vol.36 (2), p.143-159
• Main Authors: Zheng, Yongguang, Gong, Yanduo, Chen, Jiong, Tian, Fuyou
• Format: Article
• Language: English
• Subjects: Atmospheric precipitations; Atmospheric Sciences; Climate and Weather Extremes; Coastal zone; Convective precipitation; Diurnal variations; Earth and Environmental Science; Earth Sciences; Extreme weather; Geographical variations; Geophysics/Geodesy; Hourly rainfall; Meteorology; Original Paper; Precipitation; Rain gauges; Regions; Temperature; Warm seasons
• ISSN: 0256-1530; 1861-9533
• DOI: 10.1007/s00376-018-7307-3

Diurnal variations in amount, frequency and intensity of warm-season hourly precipitation (HP) at seven levels, which are defined as HP ≥ 0.1, 0.5, 1, 5, 10, 20 and 50 mm, are revealed based on no less than 30 years of hourly rain-gauge observations at national stations over central and eastern China (CEC). This study investigates the variations, relationships, differences and similarities of total, stratiform, convective and extreme HP over the entire CEC and various subregions. Results indicate that the variations in the amount and frequency of HP at the seven levels over the entire CEC all display a bimodal feature. For various regions, the variations of total HP mostly feature two peaks, while convective HP mainly occurs in the late afternoon and determines the diurnal variation of total HP intensity. On the basis of the primary peak time periods of HP frequency at all levels over different subregions, the variations can be classified into three main categories: late-afternoon primary peak, nocturnal primary peak, and time-shifting primary peak. However, the variations over some coastal regions like the Liaodong Peninsula, the Shandong Peninsula, and the coastal regions of Guangdong, distinctly differ from those over their corresponding larger regions. Overall, the normalized diurnal variation amplitude of amount and frequency increases with the increasing HP intensity; convective precipitation can be represented by HP ≥ 10 mm; and the intensity of HP ≥ 50 mm is slightly larger during the nighttime than during the daytime over the entire CEC. In northern China, diurnal variation in HP ≥ 5 mm can represent well that in convective precipitation.