Spatiotemporal Characteristics of Rainfall over Different Terrain Features in the Middle Reaches of the Yangtze River Basin during the Warm Seasons of 2016–20

IF 6.5 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Advances in Atmospheric Sciences Pub Date : 2024-03-05 DOI:10.1007/s00376-023-3034-5
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Abstract

Based on hourly rain gauge data during May–September of 2016–20, we analyze the spatiotemporal distributions of total rainfall (TR) and short-duration heavy rainfall (SDHR; hourly rainfall ⩾ 20 mm) and their diurnal variations over the middle reaches of the Yangtze River basin. For all three types of terrain (i.e., mountain, foothill, and plain), the amount of TR and SDHR both maximize in June/July, and the contribution of SDHR to TR (CST) peaks in August (amount: 23%; frequency: 1.74%). Foothill rainfall is characterized by a high TR amount and a high CST (in amount); mountain rainfall is characterized by a high TR frequency but a small CST (in amount); and plain rainfall shows a low TR amount and frequency, but a high CST (in amount). Overall, stations with high TR (amount and frequency) are mainly located over the mountains and in the foothills, while those with high SDHR (amount and frequency) are mainly concentrated in the foothills and plains close to mountainous areas. For all three types of terrain, the diurnal variations of both TR and SDHR exhibit a double peak (weak early morning and strong late afternoon) and a phase shift from the early-morning peak to the late-afternoon peak from May to August. Around the late-afternoon peak, the amount of TR and SDHR in the foothills is larger than over the mountains and plains. The TR intensity in the foothills increases significantly from midnight to afternoon, suggesting that thermal instability may play an important role in this process.

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2016-20 年暖季长江流域中游不同地形特征的降雨时空特征
摘要 基于2016-20年5-9月的小时雨量计资料,分析了长江中游流域总降雨量(TR)和短时强降雨量(SDHR;小时降雨量⩾ 20 mm)的时空分布及其昼夜变化。在所有三种地形(即山地、山麓和平原)中,TR 和 SDHR 的降雨量均在 6-7 月达到最大值,SDHR 对 TR 的贡献(CST)在 8 月达到峰值(降雨量:23%;频率:1.74%)。山麓降雨的特点是 TR 量大,CST(以量计)高;山区降雨的特点是 TR 频率高,CST(以量计)小;平原降雨的特点是 TR 量和频率低,CST(以量计)高。总体而言,TR(降雨量和降雨频率)高的站点主要分布在山区和山麓,而 SDHR(降雨量和降雨频率)高的站点主要集中在山麓和靠近山区的平原。在这三种地形中,TR 和 SDHR 的昼夜变化都呈现出双峰现象(清晨弱,午后强),并且在 5 月至 8 月期间呈现出从清晨峰值到午后峰值的相位变化。在下午晚高峰前后,山麓地区的 TR 和 SDHR 量大于山区和平原地区。山麓地区的 TR 强度从午夜到下午显著增加,表明热不稳定性可能在这一过程中发挥了重要作用。
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来源期刊
Advances in Atmospheric Sciences
Advances in Atmospheric Sciences 地学-气象与大气科学
CiteScore
9.30
自引率
5.20%
发文量
154
审稿时长
6 months
期刊介绍: Advances in Atmospheric Sciences, launched in 1984, aims to rapidly publish original scientific papers on the dynamics, physics and chemistry of the atmosphere and ocean. It covers the latest achievements and developments in the atmospheric sciences, including marine meteorology and meteorology-associated geophysics, as well as the theoretical and practical aspects of these disciplines. Papers on weather systems, numerical weather prediction, climate dynamics and variability, satellite meteorology, remote sensing, air chemistry and the boundary layer, clouds and weather modification, can be found in the journal. Papers describing the application of new mathematics or new instruments are also collected here.
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