Journal of Arid Meteorology ›› 2022, Vol. 40 ›› Issue (2): 222-233.DOI: 10.11755/j.issn.1006-7639(2022)-02-0222
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YANG Xia1(), XU Tingting1, ZHANG Linmei1, HUA Ye1, ZHOU Hongkui2
Received:
2021-01-22
Revised:
2021-03-19
Online:
2022-04-30
Published:
2022-05-10
作者简介:
杨霞(1980— ),女,甘肃武威人,硕士,正研级高级工程师,主要从事灾害性天气机理和预报技术研究. E-mail: Yangxia921@163.com。
基金资助:
CLC Number:
YANG Xia, XU Tingting, ZHANG Linmei, HUA Ye, ZHOU Hongkui. Characteristics and differences of rainstorm in the southern Xinjiang during warm season under different climatic backgrounds[J]. Journal of Arid Meteorology, 2022, 40(2): 222-233.
杨霞, 许婷婷, 张林梅, 华烨, 周鸿奎. 不同气候背景下南疆暖季暴雨特征和差异[J]. 干旱气象, 2022, 40(2): 222-233.
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URL: http://www.ghqx.org.cn/EN/10.11755/j.issn.1006-7639(2022)-02-0222
Fig.1 The terrain (the shadow, Unit: m, the same as below) and distribution of meteorological stations (the red dots are the capital sites, the green dots are the mountain sites, the blue dots are plain sites) in the southern Xinjiang
时段 | 暴雨日数/ d | 暴雨站次 | 暴雨雨量/ mm | 暴雨强度/ (mm·d-1) | 暴雨雨量占 总降水比例/% |
---|---|---|---|---|---|
暖干期 | 47.3 | 64 | 2051.8 | 31.1 | 10.0 |
暖湿期 | 62.3 | 89 | 2932.7 | 32.7 | 10.6 |
Tab.1 The rainstorm days, rainstorm stations, rainstorm rainfall, rainstorm intensity and proportion of rainstorm rainfall in total precipitation in southern Xinjiang in the warm-dry periods and the warm-wet periods from May to September during 1961-2020
时段 | 暴雨日数/ d | 暴雨站次 | 暴雨雨量/ mm | 暴雨强度/ (mm·d-1) | 暴雨雨量占 总降水比例/% |
---|---|---|---|---|---|
暖干期 | 47.3 | 64 | 2051.8 | 31.1 | 10.0 |
暖湿期 | 62.3 | 89 | 2932.7 | 32.7 | 10.6 |
Fig.2 The interdecadal variation of rainstorm days (a), rainstorm stations (b), rainstorm rainfall (c), daily rainstorm intensity (d) and proportion of rainstorm rainfall in total precipitation (e) in the southern Xinjiang from May to September during 1961-2020
Fig.3 The spatial distribution of accumulated rainstorm days (the clolor dots) in the southern Xinjiang during the warm season (Unit: d) (a) the 1960s, (b) the 1970s, (c) the 1980s, (d) the 1990s, (e) the 2000s, (f) the 2010s, (g) the warm-dry periods, (h) the warm-wet periods
Fig.4 The spatial distribution of accumulated rainstorm rainfall (the clolor dots) in the southern Xinjiang during the warm season (Unit: mm) (a) the 1960s, (b) the 1970s, (c) the 1980s, (d) the 1990s, (e) the 2000s, (f) the 2010s, (g) the warm-dry periods, (h) the warm-wet periods
Fig.5 The spatial distribution of rainstorm intensity (the clolor dots) in the southern Xinjiang during the warm season (Unit: mm·d-1) (a) the 1960s, (b) the 1970s, (c) the 1980s, (d) the 1990s, (e) the 2000s, (f) the 2010s, (g) the warm-dry periods, (h) the warm-wet periods
Fig.6 The spatial distribution of percentage of rainstorm rainfall in total precipitation (the clolor dots) in the southern Xinjiang during the warm season (Unit: %) (a) the 1960s, (b) the 1970s, (c) the 1980s, (d) the 1990s, (e) the 2000s, (f) the 2010s, (g) the warm-dry periods, (h) the warm-wet periods
时期 | 低槽型暴雨 | 低涡型暴雨 | |||
---|---|---|---|---|---|
发生次数/次 | 占比/% | 发生次数/次 | 占比/% | ||
暖干期 | 12 | 41.4 | 17 | 58.6 | |
暖湿期 | 37 | 82.2 | 8 | 17.8 |
Tab.2 The statistics of rainstorm processes of different types in the southern Xinjiang in the warm-dry periods and the warm-wet periods from May to September during 1961-2020
时期 | 低槽型暴雨 | 低涡型暴雨 | |||
---|---|---|---|---|---|
发生次数/次 | 占比/% | 发生次数/次 | 占比/% | ||
暖干期 | 12 | 41.4 | 17 | 58.6 | |
暖湿期 | 37 | 82.2 | 8 | 17.8 |
Fig.7 The composition of geopotential height field (blue lines, Unit: dagpm), wind field (black wind barbs, Unit: m·s-1) at 500 hPa and wind field at 850 hPa (red wind barbs, only plotting wind speed greater than or equal to 4 m·s-1) of low trough rainstorm (a, c) and low vortex rainstorm (b, d) in the warm-dry periods (a, b) and the warm-wet periods (c, d) in the southern Xinjiang (the gray shaded area for terrain greater than or equal to 1500 m, the same as below)
Fig.8 The difference of geopotential height field (color shaded area, Unit: gpm), flow field (black line) at 500 hPa and wind field at 850 hPa (red wind barbs) of low trough rainstorm (a) and low vortex rainstorm (b) in the warm-wet periods and the warm-dry periods in the southern Xinjiang
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