[1]Bluestein H B, Jain M H, 1985. Formation of mesoscale lines of precipitation:Severe squall lines in Oklahoma during the spring[J]. J Atmos Sci, 42(16):1711-1732.
[2]Bluestein H B, Marx G T, Jain M H, 1987. Formation of mesoscale lines of precipitation:Non-Severe squall lines in Oklahoma during the spring[J]. Mon Wea Rev, 115(11):2719-2727.
[3]Fujita T T, 1955. Results of detailed synoptic studies of squall lines[J]. Tellus, 7(4):405-436.
[4]Fujita T T, 1978. Manual of downburst identification for project NIMROD[C]//SMRP Research Paper 156, University of Chicago, 104.
[5]Takemi T, 2006. Impacts of moisture profile on the evolution and organization of midlatitude squall lines under various shear conditions[J]. Atmos Res, 82(1/2):37-54.
[6]Weisman M L, Rotunno R, 2004. "A theory for strong long-lived squall lines" revisited[J]. J Atmos Sci, 61(4):361-382.
[7]Chen M X, Wang Y C, 2012. Numerical simulation study of interactional effects of the low-level vertical wind shear with the cold pool on a squall line evolution in North China[J]. Acta Meteor Sinica, 70(3):371-386.<br/>陈明轩, 王迎春, 2012.低层垂直风切变和冷池相互作用影响华北地区一次飑线过程发展维持的数值模拟[J].气象学报, 70(3):371-386.
[8]Chen T, Dai K, Zhang F H, 2013. Study on ambient condition and initialization mechanism of convection in a severe squall line storm event in North China[J]. Meteor Mon, 39(8):945-954.<br/>陈涛, 代刊, 张芳华, 2013.一次华北飑线天气过程中环境条件与对流发展机制研究[J].气象, 39(8):945-954.
[9]Ding Y H, 1991. Advanced synoptic meteorology[M]. Beijing:China Meteorological Press.<br/>丁一汇, 1991.高等天气学[M].北京:气象出版社.
[10]Jin L, Zhao K, Xie L P, et al, 2013. Radar observation analysis on structure and evolution mechanism of a bow echo[J]. J Meteor Sci, 33(6):591-601.<br/>金龙, 赵坤, 谢利平, 等, 2013.一次弓形回波结构和演变机制的观测分析[J].气象科学, 33(6):591-601.
[11]Li H Z, Cai Z Y, Xu Y T, 1999. A numerical experiment of topographic effect on genesis of the squall line in North China[J]. Chinese J Atmos Sci, 23(6):713-721.<br/>李鸿洲, 蔡则怡, 徐元泰, 1999.华北强飑线生成环境与地形作用的数值试验研究[J].大气科学, 23(6):713-721.
[12]Li Z, Li G C, Liu L P, et al, 2017. The optimal identification method of squall line and thunderstorm winds analysis[J]. Plateau Meteor, 36(3):801-810. DOI:10.7522/j.issn. 1000-0534.2016.00040.<br/>李哲, 李国翠, 刘黎平, 等, 2017.飑线优化识别及雷暴大风分析[J].高原气象, 36(3):801-810.
[13]Liang J Y, Sun J H, 2012. The formation mechanism of damaging surface wind during the squall line in June 2009[J]. Chinese J Atmos Sci, 36 (2):316-336.<br/>梁建宇, 孙建华, 2012.2009年6月一次飑线过程灾害性大风的形成机制[J].大气科学, 36(2):316-336.
[14]Liao X N, Yu X D, Wang Y C, 2008. Analysis on an exceptionally strong wind gust event in Beijing[J]. Plateau Meteor, 27(6):1350-1362.<br/>廖晓农, 俞小鼎, 王迎春, 2008.北京地区一次罕见的雷暴大风过程特征分析[J].高原气象, 27(6):1350-1362.
[15]Liu Y, 2005. Effect of jet sub-circulation on a local lasting heavy rainstorm[J]. Meteor Sci Technol, 33(3):214-217.<br/>刘勇, 2005.急流次级环流对局地持续强风暴天气的作用[J].气象科技, 33(3):214-217.
[16]Lu Y Q, Cao Y C, Zhang F, et al, 2016. The prediction and forewarning system as well as weather characteristics analyses of hail in the East of Gansu[J]. Plateau Meteor, 35(6):1565-1576. DOI:10.7522/j.issn. 1000-0534.2015.00116.<br/>路亚奇, 曹彦超, 张峰, 等, 2016.陇东冰雹天气特征分析及预报预警[J].高原气象, 35(6):1565-1576.
[17]Ma Z Y, Su L M, Chen Y, et al, 2014. Characteristics of mesoscale and microscale systems during a severe squall line process[J]. Meteor Mon, 40(8):916-929.<br/>马中元, 苏俐敏, 谌芸, 等, 2014.一次强飑线及飑前中小尺度系统特征分析[J].气象, 40(8):916-929.
[18]Sun J H, Zheng L L, Zhao S X, 2014. Impact of moisture on the organizational mode and intensity of squall lines determined through numerical experiments[J]. Chinese J Atmos Sci, 38(4):742-755.<br/>孙建华, 郑淋淋, 赵思雄, 2014.水汽含量对飑线组织结构和强度影响的数值试验[J].大气科学, 38(4):742-755.
[19]Wang X M, Yu X D, Zhou X G, et al, 2012. Study on the formation and evolution of '6.3' damage wind[J]. Plateau Meteor, 31(2):504-514.<br/>王秀明, 俞小鼎, 周小刚, 等, 2012. "6·3"区域致灾雷暴大风形成及维持原因分析[J].高原气象, 31(2):504-514.
[20]Wu H Y, Chen H S, Jiang Y F, et al, 2013. Observation and simulation analyses on dynamical structure features in a severe squall line process on 3 June 2009[J]. Plateau Meteor, 32(4):1084-1094. DOI:10.7522/j.issn. 1000-0534.2012.00102.<br/>吴海英, 陈海山, 蒋义芳, 等, 2013. "090603"强飑线过程动力结构特征的观测与模拟分析[J].高原气象, 32(4):1084-1094.
[21]Wu Z F, Pang G Q, He H Q, et al, 2014. Comparative analysis of environmental conditions and structural features for the left moving supercell and the supercell in squall line in April 2012 Guangdong[J]. Meteor Mon, 40(6):655-667.<br/>伍志芳, 庞古乾, 贺汉青, 等, 2014.2012年4月广东左移和飑线内超级单体的环境条件和结构对比分析[J].气象, 40(6):655-667.
[22]Xu X H, Yu X, Zhu Y N, et al, 2012. Analysis on satellite retrieval of cloud structure in a severe squall Line process[J]. Plateau Meteor, 31(1):258-268.<br/>徐小红, 余兴, 朱延年, 等, 2012.一次强飑线云结构特征的卫星反演分析[J].高原气象, 31(1):258-268.
[23]Yu X D, Yao X P, X T N, et al, 2006. The principle and application of Doppler weather radar[M]. Beijing:China Meteorological Press.<br/>俞小鼎, 姚秀萍, 熊廷南, 等, 2006.多普勒天气雷达原理与业务应用[M].北京:气象出版社.
[24]Zhang J J, Wang Y Q, Zhong W, 2016. Impact of vertical wind shear and moisture on the organization of squall lines[J]. Chinese J Atmos Sci, 40(4):689-702.<br/>张建军, 王咏青, 钟玮, 2016.飑线组织化过程对环境垂直风切变和水汽的响应[J].大气科学, 40(4):689-702.
[25]Zhang P Y, 1983. Vertical airflow characteristics of squall-line hailstorm at different developmental stages[J]. Plateau Meteor, 2(3):40-48.<br/>张沛源, 1983.飑线雹暴不同发展阶段的垂直流场特征[J].高原气象, 2(3):40-48.
[26]Zhang T F, Duan X, Lu Y B, et al, 2006. Circulation background for a severe convective hailstorm weather process in Yunnan and its Doppler radar echo features[J]. Plateau Meteor, 25(3):531-538.<br/>张腾飞, 段旭, 鲁亚斌, 等, 2006.云南一次强对流冰雹过程的环流及雷达回波特征分析[J].高原气象, 25(3):531-538.
[27]Zhang T F, Zhang J, Yin L Y, 2013. Analyses on lightning feature and formation condition for a thunderstorm process in Yunnan[J]. Plateau Meteor, 32(1):268-277. DOI:10.7522/j.issn. 1000-0534.2012.00026.<br/>张腾飞, 张杰, 尹丽云, 2013.云南一次秋季雷暴过程的闪电特征及形成条件分析[J].高原气象, 32(1):268-277.
[28]Zhang X K, Chen J B, Yu Y, et al, 2017. Study on the micrometeorological characteristics over the Loess Plateau under the influence of thunderstorm[J]. Plateau Meteor, 36(2):384-394. DOI:10.7522/j.issn. 1000-0534.2017.00002.<br/>张新科, 陈晋北, 余晔, 等, 2017.雷暴系统影响下的黄土高原塬区微气象特征研究[J].高原气象, 36(2):384-394.
[29]Zheng Y Y, Zhang X C, Zhu H F, et al, 2014. Study of squall line genesis with northeast cold vortex[J]. Plateau Meteor, 33(1):261-269. DOI:10.7522//j.issn. 1000-0534.2013.00005.<br/>郑媛媛, 张雪晨, 朱红芳, 等, 2014.东北冷涡对江淮飑线生成的影响研究[J].高原气象, 33(1):261-269.
[30]Zhuang W, Liu L P, Bo Z H, et al, 2010. Study of the mesoscale wind field structure of a strong squall line in the Xinjiang Uygur Autonomous Region based on the dual-Doppler radar observations[J]. Acta Meteor Sinica, 68(2):224-234. DOI:10.11676/qxxb2010.023.<br/>庄薇, 刘黎平, 薄兆海, 等, 2010.新疆一次强飑线过程双多普勒雷达观测的中尺度风场结构分析[J].气象学报, 68(2):224-234.