Climatology and Hydrology

Diurnal variation characteristics and north-south differences of precipitation in warm season in Shaanxi Province

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  • 1 Shaanxi Meteorological Service Centre,Xi’an 710014,Shaanxi,China;
    2 Shaanxi Meteorological Observatory,Xi’an 710014,Shaanxi,China

Received date: 2018-11-09

  Revised date: 2019-03-22

  Online published: 2020-11-18

Abstract

Using the combination of data on hourly rainfall from automatic stations and Climate Prediction Center morphing method satellite data from 2008 to 2015,the diurnal variations and differences between the amount of precipitation as well as the frequency and intensity of precipitation in southern and northern Shaanxi Province,China from May to October were studied. Results show as follows:(1) From south to north,both rainfall frequency and amount decreased,with the zonal change under the topography being the most important feature. However,statistics show that precipitation intensity is higher in southwestern and northern Shaanxi and lower in central Shaanxi. The empirical orthogonal function analysis revealed that precipitation in southwestern Shaanxi showed clear night rain characteristics. (2) The diurnal variations of precipitation intensity and frequency were similar to the amount of precipitation amount southern Shaanxi. Both regions display high values from night to early morning and the lowest value around noon. The peak in precipitation amount and precipitation frequency in northern Shaanxi was primarily in the morning,while the peak in precipitation intensity appeared in the late afternoon. Diurnal variations in rainfall amount mainly came from precipitation intensity in southern Shaanxi,while diurnal variations in the north resulted from precipitation frequency. (3) Precipitation in Shaanxi varies greatly depending on what side of the north-south boundary line it falls. Precipitation south of 34°N displays obvious diurnal variation characteristics,and the precipitation is predominantly concentrated at night. There is little variation for precipitation in the central region between 34°N and 37°N,and the diurnal variation of precipitation north of the 37°N is opposite of that in southwestern Shaanxi. (4) Excluding Yulin,eastern Weinan,and Shangluo,the daytime precipitation is higher than nighttime precipitation. Precipitation in the rest of Shaanxi was significantly lower than that in the nighttime,especially in the Qinling-Daba mountainous area in southern Shaanxi,where nighttime precipitation was more than double daytime precipitation.

Cite this article

ZHANG Hong-fang, LI Jian-ke, PAN Liu-jie, LU Shan . Diurnal variation characteristics and north-south differences of precipitation in warm season in Shaanxi Province[J]. Arid Land Geography, 2020 , 43(4) : 889 -898 . DOI: 10.12118/j.issn.1000-6060.2020.04.04

References

[1] 原韦华,宇如聪,傅云飞. 中国东部夏季持续性降水日变化在淮河南北的差异分析[J]. 地球物理学报,2014,57(3):752–759.
[YUAN Weihua,YU Rucong, FU Yunfei.Study of different diurnal variations of summer long-duration rainfall between the southern and northern parts of the Huai River[J]. Chinese J. Geophys., 2014, 57(3):752–759.]
[2] 韩函,吴昊旻,黄安宁. 华北地区夏季降水日变化的时空分布特征[J].大气科学,2017, 41(2): 263–274.
[HAN Han, WU Haomin, HUANG Anning.Temporal and spatial distributions of the diurnal cycle of summer precipitation over North China[J]. Chinese Journal of Atmospheric Sciences, 2017,41(2):263–274.]
[3] 吕炯. 巴山夜雨[J]. 气象学报,1942,16(Z1):36–53.
[ LU Jiong.The Nighttime precipitation in the red Basin of Szechuan[J]. Acta Meteorologica Sinica, 1942,16(Z1):36–53.]
[4] WALLACE J M.Diurnal variations in precipitation and thunderstorm frequency over the conterminous United States[J]. Mon Wea Rev, 1975,103(5):406-419.
[5] WILLIAMS M, HOUZE R A.Satellite-observed characteristics of winter monsoon cloud clusters[J]. Mon Wea Rev, 1987,115(2):505-519.
[6] YU R C, ZHOU T J, XIONG A Y, et al.Diurnal variations of summer precipitation over contiguous China[J]. Geophys Res Lett, 2007, 34(1):L01704, doi:10.1029/2006GL028129.
[7] ZHOU T J, YU R C, CHEN H M,et al.Summer precipitation frequency, intensity, and diurnal cycle over China:A comparison of satellite data with rain gauge observations[J]. Journal of Climate, 2008, 21(16):3997–4010.
[8] CHEN H M, YU R C, LI J, et al.Why nocturnal long-duration rainfall presents an eastward-delayed diurnal phase of rainfall down the Yangtze River Valley[J]. Journal of Climate, 2010,23(4):905–917.
[9] 曹永强,张亮亮,王学凤,等. 辽宁省夏季降水量和极端雨量日时空变化特征分析[J].干旱区地理,2017,40(2):266–275.
[CAO Yongqiang,ZHANG Liangliang,WANG Xuefeng,et al.Characteristics of spatio-temporal variation of summer precipitation and extreme rainfall days in Liaoning Province in recent 54 years[J]. Arid Land Geography, 2017, 40(2):266–275.]
[10] 白爱娟,刘长海,刘晓东. TRMM多卫星降水分析资料揭示的青藏高原及其周边地区夏季降水日变化[J]. 地球物理学报, 2008,51(3):704–714.
[BAI Aijuan, LIU Changhai, LIU Xiaodong.Diurnal variation of summer rainfall over the Tibetan Plateau and its neighboring regions revealed by TRMM multi-satellite precipitation analysis[J]. Chinese Journal of Geophysics, 2008,51(3):704–714.]
[11] 白爱娟,刘晓东,刘长海. 青藏高原与四川盆地夏季降水日变化的对比分析[J]. 高原气象, 2011,30(4):852–859.
[BAI Aijuan,LIU Xiaodong, LIU Changhai.Contrast of diurnal variations of summer precipitation between the Tibetan Plateau and Sichuan Basin[J]. Plateau Meteorology,2011,30(4):852–859.]
[12] 毛江玉,吴国雄. 基于TRMM卫星资料揭示洲季风区夏季降水日变化[J]. 中国科学:地球科学,2012,42(4):564–576.
[MAO Jiangyu,WU Guoxiong.Diurnal variations of summer precipitation over the Asian monsoon region as revealed by TRMM satellite data[J]. Scientia Sinica(Terrae),2012,42(4):564–576.]
[13] 李芳洲,李江南. 基于TRMM卫星探测的南海及周边地区春夏季降水日变化特征[J].热带地理,2017,37(5):728–737.
[LI Fangzhou, LI Jiangnan.Characteristics of diurnal variations of precipitation in spring and summer over the South China Sea and its surrounding areas based on TRMM[J]. Tropical Geography, 2017, 37(5):728–737.]
[14] 宇如聪,李建,陈昊明,等. 中国大陆降水日变化研究进展[J].气象学报,2014,72(5):948–968.
[YU Rucong, LI Jian, CHEN Haoming,et al.Progress in studies of the precipitation diurnal variation over contiguous China[J]. Acta Meteorologica Sinica,2014,72(5):948–968.]
[15] 潘旸, 沈艳, 宇婧婧, 等. 基于最优插值方法分析的中国区域地面观测与卫星反演逐时降水融合试验[J]. 气象学报,2012,70(6):1381–1389.
[PAN Yang, SHEN Yan, YU Jingjing, et al.Analysis of the combined gauge-satellite hourly precipitation over China based on the OI technique[J]. Acta Meteorologica Sinica, 2012, 70(6):1381–1389.]
[16] 沈艳,潘旸,宇婧婧,等. 中国区域小时降水量融合产品的质量评估[J].大气科学学报, 2013, 36(1):37–46.
[SHEN Yan, PAN Yang, YU Jingjing, et al.Quality assessment of hourly merged precipitation product over China[J]. Transactions of Atmospheric Sciences, 2013,36(1):37–46.]
[17] 卓静,朱延年. 秦岭主脊区年降水量空间插值最优方法研究[J].干旱区地理,2017,40(3):555–563.
[ZHUO Jing, ZHU Yannian.Spatial interpolation methods of annual average precipitation on Qinling Mountains[J]. Arid Land Geography,2017,40(3):555–563.]
[18] 曾昭昭,王晓峰,任亮. 基于GWR模型的陕西秦巴山区TRMM降水数据降尺度研究[J].干旱区地理,2017,40(1):26–36.
[ZENG Zhaozhao,WANG Xiaofeng,REN Liang.Spatial downscaling of TRMM rainfall data based on GWR model for Qinling-Daba Mountains in Shaanxi Province[J]. Arid Land Geography, 2017, 40(1):26–36.]
[19] 张宏芳,潘留杰,卢珊,等. 1901—2012年陕西降水、气温变化特征[J]. 中国沙漠,2015,35(6):1674–1682.
[ZHANG Hongfang, PAN Liujie, LU Shan,et al.Variation characteristics of precipitation and air temperature from 1901 to 2012 in Shaanxi[J]. Journal of Desert Research , 2015,35(6):1674–1682.]
[20] 唐红玉,顾建峰,张焕,等. 西南地区降水日变化特征分析[J].高原气象, 2011,30(2):376–384.
[TANG Hongyu, GU Jianfeng, ZHANG Huan,et al.Analysis on diurnal variation of precipitation in southwest China[J]. Plateau Meteorology,2011,30(2):376–384.]
[21] 蔡新玲,叶殿秀,孙娴,等. 1961—2011年陕西省汛期短时降水变化特征[J]. 高原气象,2014,33(6):1618–1626.
[CAI Xinling,YE Dianxiu,SUN Xian,et al.Hourly precipitation variability features in Shaanxi Province in flood season during 1961–2011[J]. Plateau Meteorology, 2014, 33(6):1618–1626.]
[22] NORTH G R, BELL T L,CAHALAN R F,et al.Sampling errors in the estimation of empirical orthogonal function[J]. Mon Wea Rev, 1982,110(7):699–706.
[23] 卢萍,宇如聪,周天军. 2003年8月“巴蜀夜雨”过程的模拟和分析研究[J]. 气象学报,2008, 66(3):371–380.
[LU Ping,RU Yucong,ZHOU Tianjun.Numerical simulation of the mid-night rainfall over Sichuan Basin during August 2003[J]. Acta Meteorologica Sinica,2008,66(3):371–380.]
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