特强沙尘暴灾害性天气的研究及展望

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摘要总结特强沙尘暴天气的研究进展，梳理分析特强沙尘暴天气的基本特征以及动力学触发机制，提出进一步的研究问题，以期加深对特强沙尘暴天气过程机理的认识.分析结果表明特强沙尘暴天气事件的季节性分布特征显著，春季居多，且多发生在下午到傍晚时段，其典型特征为突发性、局地性，持续时间相对较短，对局地的大气环境质量短时产生重大影响.旺盛的地面混合层热对流胞运动和中尺度（反）气旋性涡旋过境是特强沙尘暴天气出现的必要条件.在沙尘源区，由于午后近地层温度升高，热对流加剧，近地层热层结极不稳定，易形成地面混合层热对流胞运动；沙尘源区的热对流胞与混合层上部的中尺度（反）气旋性涡旋耦合作用，涡量通过热对流胞下传促使近地层层结内的热对流胞发展成群发性旋转对流胞，特强沙尘暴天气出现.进一步理解特强沙尘暴的风沙流特征及能量快速耗散机制，提高预测预警能力，需要加强特沙尘暴的气象观测数据积累和多尺度数值模拟.

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	贺沅平
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关键词 ：特强沙尘暴, 动力学触发机制, 混合层, 对流胞

Abstract：The up-to-date research progress of very strong sandstorms was summarized in this study, including the characteristics and evolution mechanism of very strong sandstorms. Issues for further research have been also put forward. The very strong sandstorms showed a seasonal variation and appeared more often in spring, usually occurring from afternoon to evening suddenly and locally, with short duration. The triggering of very strong sandstorms is due to the coincidence of the upper weak air mass with certain vorticity and the developed convective bubbles in the near-surface unstable mixing layer, resulting in the onset of swirling bubbles from the common convective bubbles. The sand and dust are lifted due to the entrainment of swirling bubbles. The front of a very strong sandstorm would move slowly and finally disappeared quickly with the occurrence of secondary vortices in swirling bubbles. The occurrence of secondary vortices in swirling bubbles played a role in speeding up the energy dissipation of a very strong sandstorm. To further understand the characteristics of the wind-sand two-phase flow and the mechanism of energy dissipation of very strong sandstorms, and further improve the accuracy of sandstorm forecast, there is a need to strengthen the accumulation of meteorological observation data and the multi-scale numerical simulation of very strong sandstorms.

Key words： very strong sandstorm atmospheric dynamic triggering near-surface mixed layer convective bubbles

收稿日期: 2021-01-15

PACS:

X16

基金资助:博士后科学基金面上项目（2020M672944）；中亚大气科学研究基金（CAAS201702）

通讯作者: 顾兆林,教授,guzhaoln@mail.sysu.edu.cn E-mail: guzhaoln@mail.sysu.edu.cn

作者简介: 贺沅平(1991-),女,湖南娄底人,研究员,博士,主要从事环境多相流及数值模拟研究.发表论文20余篇.

引用本文:

贺沅平, 张云伟, 顾兆林. 特强沙尘暴灾害性天气的研究及展望[J]. 中国环境科学, 2021, 41(8): 3511-3522. HE Yuan-ping, ZHANG Yun-wei, GU Zhao-lin. Research progress of very strong sandstorm and its future research prospects. CHINA ENVIRONMENTAL SCIENCECE, 2021, 41(8): 3511-3522.

链接本文:

http://www.zghjkx.com.cn/CN/ 或 http://www.zghjkx.com.cn/CN/Y2021/V41/I8/3511

[1]	杨振华,张月霞,张全喜,等.沙尘天气PM10对多种心血管疾病日门诊人数的影响[J]. 中国环境科学, 2015,35(1):277-284. Yang Z, Zhang Y, Zhang Q, et al. Association of PM10 derived from dust events with daily outpatient number for cardiovascular diseases[J]. China Environmental Science, 2015,35(1):277-284.
[2]	张广兴,李霞.沙尘暴观测及分级标准研究现状[J]. 中国沙漠, 2003,23(5):110-115. Zhang G, Li X. Research status of sand-dust strom observation and classification standard[J]. Journal of Desert Research, 2003,23(5):110-115.
[3]	徐国昌,陈敏连,吴国雄.甘肃省"4.22"特大沙尘暴分析[J]. 气象学报, 1979,37(4):26-35. Xu G, Chen M, Wu G. On an extraordinary heavy sandstorm on April 22nd in Gansu[J]. Acta Meteorological Ainica, 1979,37(4):26-35.
[4]	马建勇,何清,杨兴华,等.塔克拉玛干沙漠区域性与塔中局地性沙尘暴特征比较[J]. 沙漠与绿洲气象, 2016,10(2):36-42. Ma J, He Q, Yang X, et al. Characteristics analysis of regional and local sandstorm over the hinterland of Taklimakan Desert:taking Tazhong as example[J]. Desert and Oasis Meteorology, 2016,10(2):36-42.
[5]	Sutton L J. Haboobs[J]. Quarterly Journal of the Royal Meteorological Society, 1925,51(213):25-30.
[6]	Idso S B, Ingram R S, Pritchard J M. An American haboob[J]. Bulletin of the American Meteorological Society, 1972,53(10):930-935.
[7]	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 Q, Qang S. On physical characteristics of heavy dust storm and its climatic effect[J]. Journal of Desert Research, 2005,25(5):675-681.
[8]	Idso S B. Dust Storms[J]. Scientific American, 1976,235(4):108-115.
[9]	Dempsey M J. Forecasting strategies for haboobs:An underreported weather phenomenon[J]. Advances in Meteorology, 2014,2014(4):1-6.
[10]	Roberts A, Knippertz P. Haboobs:Convectively generated dust storms in West Africa[J]. Weather, 2012,67(12):311-316.
[11]	Knippertz P, Trentmann J, Seifert A. High-resolution simulations of convective cold pools over the northwestern Sahara[J]. Journal of Geophysical Research Atmospheres, 2009,114(D8):D08110.
[12]	Takemi T. Structure and evolution of a severe squall line over the arid region in Northwest China[J]. Monthly Weather Review, 1998,127(6):1301-1309.
[13]	Vukovic A, Vujadinovic M, Pejanovic G, et al. Numerical simulation of "an American haboob"[J]. Atmospheric Chemistry and Physics, 2014,14(7):26175-26215.
[14]	胡隐樵,光田宁.强沙尘暴微气象特征和局地触发机制[J]. 大气科学, 1997,21(5):581-589. Hu Y, Mitsuta Y. Micrometeorological characteristics and local triggering mechanism of strong dust storm[J]. Chinese Journal of Atmospheric Sciences, 1997,21(5):581-589.
[15]	Chen F, Chen S, Zhang X, et al. Asian dust-storm activity dominated by Chinese dynasty changes since 2000BP[J]. Nature Communications, 2020,11(1):1-7.
[16]	潘耀忠,范一大,史培军,等.近50年来中国沙尘暴空间分异格局及季相分布——初步研究[J]. 自然灾害学报, 2003,12(1):1-8. Pan Y, Fan Y, Shi P, et al. Spatial variation and seasonal distribution of dust-storm in China in resent 50years:a preliminary study[J]. Journal of Natural Disasters, 2003,12(1):1-8.
[17]	尹晓惠,王式功.我国北方沙尘暴与强沙尘暴过程的分形特征及趋势预测[J]. 中国沙漠, 2007,27(1):130-136. Yi X, Wang S. Fractal characteristics and trend forecast of dust-storms and severe-dust-storms in northern China[J]. Journal of Desert Research, 2007,27(1):130-136.
[18]	赵明瑞,刘明春,钱莉,等.民勤绿洲1971~2010年沙尘暴特征及影响因素分析[J]. 沙漠与绿洲气象, 2013,7(5):35-39. Zhao M, Liu M, Qian L, et al. Variation characteristics of sandstorm from 1871 to 2010 over Minqin Oasis and its cause[J]. Desert and Oasis Meteorology, 2013,7(5):35-39.
[19]	赵明瑞,闫大同,李岩瑛,等.甘肃民勤2001~2010年沙尘暴变化特征及原因分析[J]. 中国沙漠, 2013,33(4):1144-1149. Zhao M, Yan D, Li Y, et al. Change characteristics of sandstorm frequency and its causes in 2001~2010 over Minqin, Gansu, China[J]. Journal of Desert Research, 2013,33:1144-1149.
[20]	袁国波.21世纪以来内蒙古沙尘暴特征及成因[J]. 甘肃:中国沙漠, 2017,37(6):1204-1209. Yuan G. Characteristics and cause of the sandstorm in Inner Mongolia in 2001~2015[J]. Journal of Desert Research, 2017,37(6):1204-1209.
[21]	王式功,杨德保,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 S, Yang D, Jin J, 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.
[22]	刘景涛,郑明倩.关于"黑风暴"定义的意见[J]. 内蒙古自治区:内蒙古气象, 1996,(4):5-6. Liu J, Zheng M. Opinions on the definition of "black storm"[J]. Meteorological Journal of Inner Mongolia, 1996,4:5-6.
[23]	于学军.我国人口规模及增长速度的新变化对经济社会发展的影响[J]. 人口研究, 2011,35(3):41-45. Yu X. China's population scale and the new change of growth rate to economic and social development[J]. Population Research, 2011, 35(3):41-45.
[24]	视觉中国.内蒙古突发沙尘暴,百米沙墙遮天蔽日[N]. 2016-05-24. http://slide.news.sina.com.cn/weather/slide_1_2841_99394.html?img=695013#p=2.
[25]	视觉中国.内蒙古遭强沙尘暴袭击恍如世界末日[N]. 2015-05-17. http://slide.news.sina.com.cn/c/slide_1_2841_84405.html#p=1.
[26]	社会视频.青海格尔木遭沙尘暴突袭[N]. 2015-05-26. http://tv.people.com.cn/n/2015/0526/c39805-27058530.html.
[27]	镜头故事.内蒙古额济纳遭遇强沙尘暴袭击,沙暴滚滚而来遮天蔽日[N]. 2017-08-03. https://baijiahao.baidu.com/s?id=1574686840525110&wfr=spider&for=pc.
[28]	甘肃交通广播.沙尘暴来了!昨天晚间沙尘暴突袭甘肃部分地区,一瞬间天昏地暗![N]. 2017-09-09. http://www.sohu.com/a/190750929_372695.
[29]	中国新闻网."北雪南沙"突袭天山南北新疆电力抢修恢复供电[N]. 2017-12-28. http://news.sina.com.cn/o/2017-12-28/doc-ifyqcsft7789426.shtml.
[30]	李玲萍,胡丽莉,刘维成,等.河西走廊东部夏季沙尘暴气象要素变化特征[J]. 干旱气象, 2017,35(3):427-432. Li L, Hu L, Liu W, et al. Variation characteristic of main meteorological elements during summer sand-dust storm processes in East of Hexi Corridor[J]. Journal of Arid Meteorology, 2017,35(3):427-432.
[31]	王学强.2019年春季一次强沙尘暴天气过程分析[J]. 农业灾害研究, 2020,10(5):87-88. Wang X. Analysis on the weather process of a strong sandstorm in Spring of 2019[J]. Journal of Agricultural Catastrophology, 2020, 10(5):87-88.
[32]	Heinold B, Knippertz P, Marsham J H, et al. The role of deep convection and nocturnal low-level jets for dust emission in summertime West Africa:Estimates from convection-permitting simulations[J]. Journal of Geophysical Research Atmospheres, 2013, 118(10):4385-4400.
[33]	卢琦,杨有林.全球沙尘暴警世录[M]. 北京:中国环境科学出版社, 2001,158. Lu Q, Yang Y. Warnings from global dust storm[M]. Beijing:China Environmental Science Press, 2001:157-166.
[34]	段海霞,李耀辉,蒲朝霞,等.高空急流对一次强沙尘暴过程沙尘传输的影响[J]. 中国沙漠, 2013,33(5):1461-1472. Duan H, Li Y, Pu Z, et al. The influence of high level jet on dust transportation in a sandstorm process[J]. Journal of Desert Research, 2013,33(5):1461-1472.
[35]	江吉喜,项续康,王子厚,等.以卫星资料为主的强沙尘暴超短期预报方法初探[A]. 见:方宗义编.中国沙尘暴研究[C]. 北京:气象出版社, 1997:98-102. Jing J, Xiang X, Wang Z, et al. A preliminary study on the ultra-short term prediction method of strong sandstorm based on satellite data[A]. Editor:Fang Z. Sandstorms in China[C]. Beijing:Meteorology Press, 1997:98-102.
[36]	瞿章,许宝玉,贺慧霞."930505"沙尘暴的若干启示[J]. 干旱区地理, 1994,17(1):63-67. Di Z, Xu B, He H. Some enlightenments from a sandstorm occurred in northwest China[J]. Arid Land Geography, 1994,17(1):63-67.
[37]	李彰俊,姜学恭,郝璐.沙尘暴形成及下垫面对其影响研究[M]. 北京:气象出版社, 2009,326. Li Z, Jiang X, Hao L. Sandstorm formation and its influence from underlying surface[M]. Beijing:China Meteorological Press, 2009:326.
[38]	刘春涛,程麟生.黑风暴的沙尘形成与输送参数化及中尺度数值试验[J]. 北京:气象学报, 1997,55(6):726-739. Liu C, Cheng L. Parameterization of the formation and transportion for sand-dust of the black storm and mesoscale numerical experiments[J]. Acta Meteorological Ainica, 1997,55(6):726-939.
[39]	狄潇泓,刘新伟,沙宏娥,等.河西走廊一次强沙尘暴动力机制分析[J]. 干旱区资源与环境, 2016,30(8):145-151. Di X, Liu X, Sha H, et al. Dynamic mechanism of a severe sandstorm occurred in the Hexi Corridor[J]. Journal of Arid Land Resources and Environment, 2016,30(8):145-151.
[40]	马丽云,李帅.基于FY-2气象卫星的塔克拉玛干沙漠黑风暴天气判识方法研究[J]. 干旱区研究, 2016,33(1):59-66. Ma L, Li S. Identification of dark sandstorm process in Taklamakan Desert based on FY-2meteorological satellite data[J]. Arid Zone Research, 2016,33(1):59-66.
[41]	Jiang X G, Shen J G, Liu J T, et al. Numerical simulation of synoptic condition on a severe sand dust storm[J]. Water Air & Soil Pollution Focus, 2003,3(2):191-212.
[42]	Raman A, Arellano Jr A F, Brost J J. Revisiting haboobs in the southwestern United States:An observational case study of the 5July 2011 Phoenix dust storm[J]. Atmospheric Environment, 2014,89:179-188.
[43]	Marsham J H. The importance of the representation of deep convection for modeled dust-generating winds over West Africa during summer[J]. Geophysical Research Letters, 2011,38:L16803.
[44]	宋振鑫,程麟生."93.5"黑风暴扰动能源的诊断分析[J]. 兰州大学学报:自然科学版, 1997,33(4):116-122. Song Z, Cheng L. Diagnostic analysis of the perturbation sources on the "93.5" black storm[J]. Journal of Lanzhou University (Natural Sciences), 1997,33(4):116-122.
[45]	程麟生,马艳."93.5"黑风暴发展结构和不同模式分辨率的数值试验[J]. 应用气象学报, 1996,(4):385-395. Cheng L, Ma Y. The developing structure of a black storm and its numerical experiment of different model resolution. Quarterly Journal of Applied Meteorology, 1996,7(4):385-395.
[46]	张小玲,程麟生."93.5"黑风暴期间中尺度涡旋发生发展的涡源诊断[J]. 兰州大学学报:自然科学版, 1997,(4):123-131. Zhang X, Cheng L. Diagnosis of vorticity source for the genesis and development of mesoscale vortex during "93.5" black storm[J]. Journal of Lanzhou University (Natural Sciences), 1997,33:123-131.
[47]	胡隐樵,光田宁.强沙尘暴发展与干飑线——黑风暴形成的一个机理分析[J]. 高原气象, 1996,15(2):178-185. Hu Y, Mitsuta Y. Development of the strong dust storm and dry squall line-a mechanism analysis on generation black storm[J]. Plateau Meteorology, 1996,15(2):178-185,T003.
[48]	马禹,王旭,肖开提,等.天山北麓一例黑风暴天气的成因[J]. 北京大学学报(自然科学版), 2006,42(3):343-350. Ma Y, Wang X, Xiao K, et al. A case study of a black storm at the northern foothills of Tianshan Mountains[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2006,42:343-350.
[49]	He Y, Gu Z, Shui Q, et al. RANS simulation of local strong sandstorms induced by a cold pool with vorticity[J]. Atmosphere, 2020,11(4):321.
[50]	顾润源,陈磊,周伟灿,等.一次强沙尘暴的近地层气象要素及内部热力、动力结构特征[J]. 大气科学学报, 2014,37(4):414-424. Gu R, Chen L, Zhou W, et al. The surface layer meteorological parameters and the thermos-dynamical structure of a severe sandstorm[J]. Transactions of Atmospheric Sciences, 2014,37(4):414-424.
[51]	李岩瑛,张强,李耀辉,等.水平螺旋度与沙尘暴的动力学关系研究[J]. 地球物理学报, 2008,51(3):692-703. Li Y, Zhang Q, Li Y, et al. Dynamic relationships between the horizontal helicity and the sandstorm[J]. Chinese Journal of Geophysics, 2008,51(3):692-703.
[52]	托马斯·沃纳.沙漠气象学[M]. 北京:气象出版社, 2008:12-36. Warner T. Desert Meteorology[M]. Beijing:Meteorology Press, 2008:12-36.
[53]	Oke A M C, Tapper N J, Dunkerley D. Willy-willies in the Australian landscape:The role of key meteorological variables and surface conditions in defining frequency and spatial characteristics[J]. Journal of Arid Environments, 2007,71(2):201-215.
[54]	Huang Q, Marsham J, Tian W, et al. Large eddy simulation of dust-uplift by haboob density currents[J]. Atmospheric Environment, 2018,179:31-39.
[55]	顾兆林.风扬粉尘——近地层湍流与气固两相流[M]. 北京:科学出版社, 2010:28-32. Gu Z. Wind-blown sand:near-surface turbulence and gas-solid two-phase flow[M]. Beijing:Science Press, 2010:28-32.
[56]	高庆先,任阵海.沙尘暴——自然对人类的报复[M]. 北京:化学工业出版社, 2002:178. Gao Q, Ren Z. Sandstorms:the revenges that the nature pay back to human beings[M]. Beijing:Chemical Industrial Press, 2002:178.
[57]	Decroix D S, Lin Y L, Schowalter D G. Cellular convection embedded in the convective planetary boundary layer surface layer[J]. Journal of Wind Engineering & Industrial Aerodynamics, 1997,67-68(2):387-401.
[58]	Kanak K M, Lilly D K, Snow J T. The formation of vertical Vortices in the convective boundary layer[J]. Quarterly Journal of the Royal Meteorological Society, 2000,126(569):2789-2810.
[59]	赵永志.尘卷风形成、演化及结构的理论分析和数值研究[D]. 西安:西安交通大学, 2004. Zhao Y. Theoretical analysis and numerical simulations for the formation, evolution and structure of dust devil[D]. Xi'an:Xi'an Jiaotong University, 2004.
[60]	Gu Z L, Qiu J, Zhao Y Z, et al. Analysis on dust devil containing loess dusts of different sizes[J]. Aerosol & Air Quality Research, 2008, 8(1):65-77.
[61]	Spiga A, Barth E, Gu Z, et al. Large-eddy simulations of dust devils and convective vortices[J]. Space Science Reviews, 2016,203:1-31.
[62]	Gu Z, Zhao Y, Li Y, et al. Numerical simulation of dust lifting within dust devils-simulation of an intense vortex[J]. Journal of the Atmospheric Sciences, 2006,63(10):2630-2641.
[63]	王式功,杨德保,孟梅芝,等.甘肃河西"5.5"黑风天气系统结构特征及其成因分析[J]. 干旱气象, 1993,11(3):30-33. Wang S, Yang D, Meng M, et al. Structural characteristics and cause analysis of "5.5" black storm weather system in Hexi, Gansu Province[J]. Arid Meteorology, 1993,11(3):30-33.
[64]	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):349-356. Wang S, Dong G, Chen H, et al. Advances in studying sand-dust storms of China[J]. Journal of Desert Research, 2000,20(4):349-356.
[65]	李岩瑛,李耀辉,罗晓玲,等.河西走廊东部沙尘暴预报方法研究[J]. 中国沙漠, 2004,24(5):607-610. Li Y, Zhang Q, Li Y, et al. Dynamic relationships between the horizontal helicity and the sandstorm[J]. Chinese Journal of Geophysics, 2008,51(3):692-703.
[66]	Gao T, Han J. Evolutionary characteristics of the atmospheric circulations for frequent and infrequent dust storm springs in northern China and the detection of potential future seasonal forecast signals[J]. Meteorological Applications, 2010,17:76-87.
[67]	郭萍萍,殷雪莲,刘秀兰,等.河西走廊中部一次特强沙尘暴天气特征及预报方法研究[J]. 干旱气象, 2011,29(1):110-115. Guo P, Yin X, Liu X, et al. Analysis of a heavy dust storm occurred in middle part of Hexi Corridor and forecast methods study for dust storm weather[J]. Arid Meteorology, 2011,29(1):110-115.
[68]	刘开福,陈雷.黑风暴前6小时的天气系统跃变[J]. 干旱气象, 2001,19(2):45-47. Liu K, Chen L. Six hours abrupt change of the weather before black sandstorm[J]. Arid Meteorology, 2001,19(2):45-47.
[69]	宋振鑫.国家级沙尘天气数值预报业务系统[C]//中国气象学会2004年年会, 2004. Song Z. National dust weather numerical prediction system[C]//Annual Meeting of Chinese Meteorological Society, 2004.
[70]	卢晶晶,赵琳娜,杜秉玉.2004年春季一次较强沙尘暴的实时预报与特征分析[J]. 气候与环境研究, 2007,(2):188-198. Lu J, Zhao L, Du B. The real time numerical prediction and characteristics of a severe dust storm covers China in the spring of 2004[J]. Climatic and Environmental Research, 2007,(2):188-198.
[71]	段海霞,郭铌,霍文,等.GRAPES-SDM沙尘模式预报与卫星遥感监测结果对比[J]. 中国沙漠, 2014,34(6):1617-1623. Duan H, Guo N, Huo W, et al. The comparison of the prediction efficiency of GRAPES-SDM dust-storm model and the satellite remote sensing monitoring[J]. Journal of Desert Research, 2014, 34(6):1617-1623.
[72]	段海霞,赵建华,李耀辉,等.近年来GRAPES-SDM沙尘模式预报效果检验评估[J]. 中国沙漠, 2013,33(1):214-222. Duan H, Zhao J, Li Y, et al. A verification on the prediction efficiency of GRAPES-SDM model used in recent years[J]. Journal of Desert Research, 2013,33(1):214-222.
[73]	Raman A. Modeling and data analysis of 2011 Phoenix dust storm[C]. 93rd AMS annual meeting, 2013.
[74]	Eltahan M, Shokr M, Sherif A O. Tuning dust schemes in weather research forecast (WRF-Chem) for simulating severe dust storm events over Egypt[C]. AGU Conference, 2017.
[75]	Karegar E, Hamzeh N H, Jamali J B, et al. Numerical simulation of extreme dust storms in east of Iran by the WRF-Chem model[J]. Natural Hazards, 2019,99(31):769-796.
[76]	Vukovic A J, Pejanovic G, Vujadinovic M, et al. Dust storm of July 5th 2011, Phoenix, Arizona:Numerical simulation[C]. Agu Fall Meeting, 2011.
[77]	Lee P, Baker B, Tong D, et al. Dynamic coupling of the NMMB and CMAQ models through the U.S. national unified operational prediction capability (NUOPC)[C]. International Technical Meeting on Air Pollution Modelling and its Application, 2018.