河西走廊东部沙尘暴特征及地面气象因素影响机制

Abstract

Abstract:

Change characteristics and mechanism of sandstorm frequency in east Hexi Corridor during the period of 1961-2015 were analyzed using the meteorological and sandstorm data from Minqin, Liangzhou and Yongchang. The meteorological data, including the monthly air and ground temperature, precipitation, maximum frozen soil depth, snow cover duration and depth, wind speed and gale days, were from representative Minqin Meteorological Station. The results showed that there were the obvious daily, monthly and seasonal variations in sandstorm frequency and occurrence time. Sandstorm occurred mainly in April and spring and was the least in September and autumn, and its occurring frequency was the highest in the afternoon and evening but the lowest in the early morning. The spring sandstorm frequency began to increase in the morning, the autumn and winter one began to increase at noon, and the summer one began to increase in the afternoon. The sandstorm frequency with 60-180-min duration was the highest in east Hexi Corridor, and it with 1~30-min duration was the highest in summer. The long-duration sandstorm began to increase in the morning, and the short-time one occurred mainly in the afternoon and evening. The monthly and seasonal variation of sandstorm frequency was the most significant in April and spring, and it was the lowest in September and autumn. In recent 55 years from 1961 to 2015, the sandstorm frequency was in a decrease trend due to the reduction of gale days and wind speed, increase of ground temperature, air temperature and precipitation, and improvement of ecological environment of underlying surface.

Key words: sandstorm, meteorological factor, temperature, precipitation, east Hexi Corridor

LI Ling-ping, LI Yan-ying, SUN Zhan-feng, WANG Rong-zhe. Sandstorm and Its Affecting Meteorological Factors in East Hexi Corridor[J].Arid Zone Research, 2019, 36(6): 1457-1465.

References 35

[1]	中国气象局.地面气象观测规范[M].北京:气象出版社,2003.[China Meteorological Administrator.The Criterion of Surface Meteorological Observation[M].Beijing:Meteorological Press,2003.]
[2]	朱炳海,王鹏飞,束家鑫.气象学词典[M].上海:上海辞书出版社,1985.[Zhu Binghai,Wang Pengfei,Shu Jiaxin.Meteorology Dictionary[M].Shanghai:Shanghai Dictionary Publishing House,1985.]
[3]	王式功,王金艳,周自江,等.中国沙尘天气的区域特征[J].地理学报,2003,58(2):193-200.[Wang Shigong,Wang Jinyan,Zhou Zijiang,et al.Regional characteristics of dust events in China[J].Acta Geaographica Sinica,2003,58(2):193-200.]
[4]	周自江.近45 年中国扬沙和沙尘暴天气[J].第四纪研究,2001,21(1):9-17.[Zhou Zijiang.Blowing-sand and sandstorm in China in recent 45 years[J].Quaternary Sciences,2001,21(1):9-17.]
[5]	王式功,董光荣,陈惠忠,等.沙尘暴研究的进展[J].中国沙漠,2000,20(4)：349-358.[Wang Shigong,Dong Guangrong,Chen Huizhong,et al.Advances in studying sand-dust storms of China[J].Journal of Desert Research,2000,20(4):349-358.]
[6]	方宗义,朱福康.中国沙尘暴研究[M].北京：气象出版社，1997:1-10.[Fang Zongyi,Zhu Fukang.Study on Sandstorm in China[M].Beijing:Meteorological Press,1997:1-10.]
[7]	张瑞军,何清,孔丹,等.近几年国内沙尘暴研究的初步评述[J].干旱气象,2007,25(4):88-94.[Zhang Ruijun,He Qing,Kong Dan,et al.Preliminary summary on sand-dust storm research in recent years in China[J].Arid Meteorology,2007,25(4):88-94.]
[8]	王式功,杨得宝,金炯,等.我国西北地区黑风暴的成因和对策[J].中国沙漠,1995,15(1):19-30.[Wang Shigong,Yang Debao,Jin Jong,et al.Study on the formative causes and countermeasures of the catastrophic sandstorm occurred in Northwest China[J].Journal of Desert Research,1995,15(1):19-30.]
[9]	王汝佛,冯强,尚可政.2010春季我国一次强沙尘暴过程分析[J].干旱区地理,2014,37(1):31-44.[Wang Rufo,Feng Qiang,Shang Kezheng.A severe sand-dust storm over China in the spring of 2010[J].Arid Land Geography,2014,37(1):31-44.]
[10]	李岩瑛,杨晓玲,王式功.河西走廊东部近50 a沙尘暴成因、危害及防御对策[J].中国沙漠,2002,22(3):283-287.[Li Yanying,Yang Xiaoling ,Wang Shigong.Cause,damage and countermeasure of sandstorm in the east of Hexi Corridor during the later 50 years[J].Journal of Desert Research,2002,22(3):283-287.]
[11]	Bonnifield M P.The Dust Bowl:Men,Dirt,and Depression[M].Albuquerque:University of New Mexico Press,1979.
[12]	Howarth W.The okies:Beyond the dust bowl[J].National Geographic,1984,166(3):322-349.
[13]	Lee J A,Gill T E,Mulligan K R.The 1930s dust bowl:The relative roles of people and the physical environment[J].Geological Society of Abstracts and Programs,1999,31(1):A11.
[14]	Stallings F L.Black Sunday:The Great Dust Storm of April 14,1935[M].Austin:Eakin Press,2001.
[15]	钱正安,宋敏红,李万元.近50年来中国北方沙尘暴的分布及变化趋势分析[J].中国沙漠,2002,22(2):106-111.[Qian Zheng’an,Song Minhong,Li Wanyuan.Analyses on distributive variation and forecast of sanddust storms in recent 50 years in North China[J].Journal of Desert Research,2002,22(2):106-111.]
[16]	蒋雨荷，王式功，靳双龙，等.中国北方一次强沙尘暴天气过程的大气污染效应[J].干旱区研究,2018,35(6):1 344-1 351.[Jiang Yuhe,Wang Shigong，Jin Shuanglong,et al.Air pollution in a strong sandstorm in north China[J].Arid Zone Research,2018,35(6):1 344-1 351.]
[17]	岳平，牛生杰，刘晓云．“7·12”特异沙尘暴成因研究[J]．干旱区研究，2005，23(3):345-349．[Yue Ping,Niu Shengjie,Liu Xiaoyun.Study on the formation causes of the peculiar dust storm occurred on July 12,2004[J].Arid Zone Research，2005，23(3):345-349.]
[18]	许东蓓,杨民,孙兰东,等.西北地区“4·18”强沙尘暴、浮尘天气成因分析[J].甘肃气象,1999,17(2):6-9.[Xu Dongbei,Yang Min,Sun Landong,et al.An cause analysis on “4·18”sandstrom and dust storm in north China[J].Gansu Meteorology,1999,17(2):6-9.]
[19]	徐启运,胡敬松.我国西北地区沙尘暴天气时空分布特征[J].应用气象学报,1998,7(4):479-482.[Xu Qiyun,Hu Jingsong.Features of spatial and temporal distributions of the dust storms in Northwest China[J].Quarterly Journal of Applied Meteorlogy,1998,7(4):479-482.]
[20]	刘洪兰,张强,张俊国,等.1960—2012年河西走廊中部沙尘暴空间分布特征和变化规律[J].中国沙漠,2014,34(4):1 102-1 108.[Liu Honglan,Zhang Qiang,Zhang Junguo,et al.Spatial distribution and variation of sand storms in the central Hexi Corridor during 1960-2012[J].Journal of Desert Research,2014,34(4):1 102-1 108.]
[21]	邱新法,曾燕,缪启龙．我国沙尘暴的时空分布规律及其源地和移动路径[J].地理学报,2001,58(3):316-322.[Qiu Xinfa,Zeng Yan,Liao Qilong.Temporal-spatial distribution as well as tracks and source areas of sand-dust storms in China[J].Acta Geographica Sinica,2001,58(3):316-322.]
[22]	钱莉,杨金虎,杨晓玲,等.河西走廊东部“2008·5·2”强沙暴成因分析[J].高原气象,2010,29(3):719-725.[Qian Li,Yang Jinhu,Yang Xiaoling,et al.Cause analysis of “2008·5·2” strong sandstorm in the eastern of Hexi Corridor[J]．Plateau Meteorology,2010,29(3):719-725.]
[23]	杨晓玲,丁文魁,王鹤龄,等.河西走廊东部沙尘暴气候特征及短时预报[J].中国沙漠,2016,36(2):449-457.[Yang Xiaoling,Ding Wenkui,Wang Heling,et al.Climatic characteristics and short-term forecast of sandstorm in east of Hexi Corridor[J].Journal of Desert Research,2016,36(2):449-457.]
[24]	江灏,吴虹,尹宪志,等.河西走廊沙尘暴的时空变化特征与其环流背景[J].高原气象,2004,23(4):820-826.[Jiang Hao,Wu Hong,Yin Xianzhi,et al.Spatial and temporal change characteristics and circulation background of sandstorm in Gansu Corridor[J].Plateau Meteorology,2004,23(4):820-826.]
[25]	张强，王胜.论特强沙尘暴(黑风)的物理特征及其气候效应[J].中国沙漠，2005,25(5):675-681.[Zhang Qiang,Wang Sheng.On physical characteristics of heavy dust storm and its climatic effect[J].Journal of Desert Research,2005,25(5):675-681.]
[26]	王劲松，李耀辉，康凤琴，等．“4·12”沙尘暴天气的数值模拟及诊断分析[J].高原气象,2004，23(1):89-96．[Wang Jinsong,Li Yaohui，Kang Fengqin，et al.Numerical simulation and diagnose analysis on“4·12”sandstorm[J].Plateau Meteorology,2004,23(1):89-96．]
[27]	董安祥，白虎志，陆登荣，等．河西走廊强和特强沙尘暴变化趋势的初步研究[J].高原气象,2003，22(4):422-425.[Dong Anxiang，Bai Huzhi，Lu Dengrong，et al．Primary study on strong and very strong dust storm trend in Hexi Passageway[J]．Plateau Meteorology，2003,22(4):422-425.]
[28]	胡泽勇,黄荣辉,卫国安,等.2000年6月4日沙尘暴过境时敦煌地面气象要素及地表能量平衡特征的变化[J].大气科学,2002,26(1):1-7.[Hu Zeyong,Huang Ronghui,Wei Guoan,et al.Variations of surface atmospheric variables and energy budget during a sandstorm passing Dunhuang on June 4 of 2000[J].Chinese Journal of Atmospheric Sciences,2002,26(1):1-7.]
[29]	牛生杰，岳平，刘晓云,等.2004年春夏季两次沙尘暴期间地面气象要素变化特征对比分析[J].中国沙漠,2007,27(6):1 067-1 071.[Niu Shengjie,Yue Ping,Liu Xiaoyun,et al.Variations of surface meteorological element during twice sandstorms passing Jiuquan on March 28 and July 12 of 2004[J].Journal of Desert Research,2007,27(6):1 067-1 071.]
[30]	赵庆云，张武，吕萍，等．河西走廊“2010·4·24”特强沙尘暴特征分析[J]．高原气象,2012,31(3):688-696.[Zhao Qingyun,Zhang Wu,Lv Ping,et al.Characteristic analysis of the sever dust event occurred in the Hexi Corridor on 24 April 2010.[J]．Plateau Meteorology,2012,31(3):688-696.]
[31]	王式功,杨德保,周玉素,等．我国西北地区“94·4”沙尘暴成因探讨[J].中国沙漠,1995,15(4):332-334.[Wang Shigong,Yang Debao,Zhou Yusu,et al.Analysis on the formative causes of sand-dust storms in the Northwest China during 3-12 April 1994[J].Journal of Desert Research,1995,15(4):332-334.]
[32]	付有智,刘坤训,丁荣,等.甘肃河西黑风成因及预报[J].气象,1994,20(12):50-53.[Fu Youzhi,Liu Kunxun,Ding Rong,et al.The causative factors and forecasting of the black storm in Hexi Corridor[J].Meteorological Monthly,1994,20(12):50-53.]
[33]	高庆先,李令军,张运刚,等.我国春季沙尘暴研究[J].中国环境科学,2000,20(6):495-500.[Gao Qingxian,Li Lingjun,Zhang Yungang,et al.Studies on the springtime dust storm of China[J].China Environmental Science,2000,20(6):495-500.]
[34]	赵建华,俞亚勋,孙国武.冻土对沙尘暴的影响研究[J].中国沙漠,2005,25(5):658-662.[Zhao Jianhua,Yu Yaxun,Sun Guowu.Influence of frozen soil on sandstorm[J].Journal of Desert Research,2005,25(5):658-662.]
[35]	李玲萍,陈英,李文莉,等.石羊河流域冬季冻土对沙尘天气的影响分析[J].土壤通报,2013,44(5):1 204-1 209.[Li Lingping,Chen Ying,Li Wenli,et al.Influence of winter maximum frozen soil depth on sand-dust weather days over Shiyang River Basin[J].Chinese Journal of Soil Science,2013,44(5):1 204-1 209.]

Sandstorm and Its Affecting Meteorological Factors in East Hexi Corridor

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