[1]Hoskins B J, Draghici I, Davies H C.1978.A new look at the <i>ω</i>-equation[J].Quart J Roy Meteor Soc, 104(1): 31-38.
[2]邓伟, 陈海波, 马振升, 等.2009.NCEP FNL全球分析资料的解码及其图形显示[J].气象与环境科学, 32(3): 78-82.
[3]Deng Wei, Chen Haibo, Ma Zhensheng, et al.2009.Decording and graphic display of the NCEP FNL global analysis data[J].Meteor Environ Sci, 32(3): 78-82.
[4]丁一汇.1989.天气动力学中的诊断分析方法[M].北京:科学出版社, 114-118.
[5]Ding Yihui.1989.Diagnostic analysis methods of synoptic dynamics[M].Beijing: Science Press, 114-118.
[6]丁一汇.2005.高等天气学 (第二版)[M].北京:气象出版社, 123-130.
[7]Ding Yihui.2005.Advanced synoptic meteorology (the second edition)[M].Beijing: China Meteorological Press, 123-130.
[8]高守亭.2007.大气中尺度运动的动力学基础及预报方法[M].北京:气象出版社, 192-196.
[9]Gao Shouting.2007.Dynamical foundation and prediction methods of mesoscale motions in the atmosphere[M].Beijing: China Meteorological Press, 192-196.
[10]何光碧, 高文良, 屠妮妮.2009.2000-2007年夏季青藏高原低涡切变线观测事实分析[J].高原气象, 28(3): 549-555.
[11]He Guangbi, Gao Wenliang, Tu Nini.2009.The observational analysis of shear line and low vortex over the Tibetan Plateau in summer from 2000 to 2007[J].Plateau Meteor, 28(3): 549-555.
[12]何光碧, 师锐.2011.夏季青藏高原不同类型切变线的动力、热力特征分析[J].高原气象, 30(3): 568-575.
[13]He Guangbi, Shi Rui.2011.Study on dynamic and thermal characteristics of different shear lines over Tibetan in summer[J].Plateau Meteor, 30(3): 568-575.
[14]何光碧, 师锐.2014.三次高原切变线过程演变特征及其对降水的影响[J].高原气象, 33(3): 615-625.
[15]He Guangbi, Shi Rui.2014.Analysis on evolution characteristics of three Plateau shearlines and their effect on precipitation[J].Plateau Meteor, 33(3): 615-625.DOI: 10.7522/j.issn.1000-0534.2013.00023.
[16]何光碧, 屠妮妮, 张利红, 等.2013.青藏高原东侧一次低涡暴雨过程地形影响的数值试验[J].高原气象, 32(6): 1546-1556.
[17]He Guangbi, Tu Nini, Zhang Lihong, et al.2013.Numerical experiment of terrain effect of vortex rainstorm process on east side of Qinghai-Xizang Plateau[J].Plateau Meteor, 32(6): 1546-1556.DOI: 10.7522/j.issn.1000-0534.2012.00150.
[18]黄楚惠, 李国平.2009.基于螺旋度和非地转湿<i><b>Q</b></i>矢量的一次东移高原低涡强降水过程分析[J].高原气象, 28(2): 319-326.
[19]Huang Chuhui, Li Guoping.2009.A case study of Plateau vortex moving east ward with heavy rainfalls based on helicity and non-Geostrophic wet <i><b>Q</b></i>-vector[J].Plateau Meteor, 28(2): 319-326.
[20]李川, 陈静, 何光碧.2006.青藏高原东侧陡峭地形对一次强降水天气过程的影响[J].高原气象, 25(3): 442-450.
[21]Li Chuan, Chen Jing, He Guangbi.2006.Impact of the steep terrain of eastern Qinghai-Xizang Plateau on the genesis and development of extreme heavy rainfall event[J].Plateau Meteor, 25(3): 442-450.
[22]刘海明, 巨克英, 张青梅, 等.2000.Q矢量及水汽通量散度在青海省1999年8月4日大降水中的释用[J].青海气象, 42(3): 2-7.
[23]Liu Haiming, Ju Keying, Zhang Qingmei, et al.2000.The interpretation of Q vector and moisture flux divergence on heavy rainfall in Qinghai Province on August 4, 1999[J].Qinghai Meteor, 42(3): 2-7.
[24]彭广, 李跃清, 郁淑华, 等.2015.青藏高原低涡切变线年鉴 (2013)[M].北京:科学出版社, 194-198.
[25]Peng Guang, Li Yueqing, Yu Shuhua, et al.2015.The Tibetan Plateau vortex and shear line yearbook (2013)[M].Beijing: Science Press, 194-198.
[26]王伏村, 许东蓓, 修韶宇, 等.2014.一次西北地区东部大暴雨的物理机制分析[J].高原气象, 33(6): 1501-1513.
[27]Wang Fucun, Xu Dongbei, Xiu Shaoyu, et al.2014.Mechanism analysis of a rainstorm occurred in the eastern part of Northwest China[J].Plateau Meteor, 33(6): 1501-1513.DOI: 10.7522/j.issn.1000-0534.2013.00104.
[28]王婧羽, 崔春光, 王晓芳, 等.2014.2012年7月21日北京特大暴雨过程的水汽输送特征[J].气象, 40(2): 133-145.
[29]Wang Jingyu, Cui Chunguang, Wang Xiaofang, et al.2014.Analysis on water vapor transport and budget of the severe torrential rain over Beijing region on 21 July 2012[J].Meteor, 40(2): 133-145.
[30]文宝安.1980.物理量计算及其在暴雨分析预报中的应用—水汽通量与水汽通量散度[J].气象, 31(6): 34-36.
[31]Wen Baoan.1980.Physical quantity calculation and application to analysis and forecast of the torrential rain—moisture flux and moisture flux divergence[J].Meteor, 31(6): 34-36.
[32]肖递祥, 屠妮妮, 祁生秀.2015.龙门山沿线暴雨过程的诊断分析及数值试验[J].高原气象, 34(1): 113-123.
[33]Xiao Dixiang, Tu Nini, Qi Shengxiu.2015.Diagnosis analysis and numerical experiments of a rainstorm case along Longmen Mountain[J].Plateau Meteor, 34(1): 113-123.DOI: 10.7522/j.issn.1000-0534.2013.00112.
[34]颜琼丹, 蔡亲波.2006.非地转湿<i><b>Q</b></i>矢量在台风"云娜"暴雨过程中的分析应用[J].热带气象学报, 22(5): 505-509.
[35]Yan Qiongdan, Cai Qinbo.2006.Application of ageostrophic wet <i><b>Q</b></i>-vector analysis in torrential rain of typhoon "Rananim"[J].J Trop Meteor, 22(5): 505-509.
[36]杨晓霞, 沈桐立, 刘还珠, 等.2006.非地转湿<i><b>Q</b></i>矢量分解在暴雨分析中的应用[J].高原气象, 25(3): 464-475.
[37]Yang Xiaoxia, Shen Tongli, Liu Huanzhu, et al.2006.Application of the wet <i><b>Q</b></i>-vector partitioning method to the diagnosis of the heavy rainstorm[J].Plateau Meteor, 25(3): 464-475.
[38]姚秀萍, 孙建元, 康岚, 等.2014.高原切变线研究的若干进展[J].高原气象, 33(1): 294-300.
[39]Yao Xiuping, Sun Jianyuan, Kang Lan, et al.2014.Advances on research of shear convergence line over Qinghai-Xizang Plateau[J].Plateau Meteor, 33(1): 294-300.DOI: 10.7522/j.issn.1000-0534.2013.00164.
[40]姚秀萍, 于玉斌.2000.非地转湿<i><b>Q</b></i>矢量及其在华北特大台风暴雨中的应用[J].气象学报, 58(4): 436-446.
[41]Yao Xiuping, Yu Yubin.2000.Non-geostrophic wet <i><b>Q</b></i>-vector analysis and its application to typhoon torrential rain[J].Acta Meteor Sinica, 58(4): 436-446.
[42]岳彩军, 李佳, 陈佩燕, 等.2013.湿<i><b>Q</b></i>矢量释用技术的改进研究[J].高原气象, 32(6): 1617-1625.
[43]Yue Caijun, Li Jia, Chen Peiyan, et al.2013.Study on improvement of moist Q-vector interpretation technique[J].Plateau Meteor, 32(6): 1617-1625.DOI: 10.7522/j.issn.1000-0534.2012.00155.
[44]岳彩军, 寿绍文, 董美莹, 等.2003.定量分析几种<i><b>Q</b></i>矢量[J].应用气象学报, 14(1): 209-213.
[45]Yue Caijun, Shou Shaowen, Dong Meiying, et al.2003.Quantitative analysis of several <i><b>Q</b></i>-vectors[J].Appl Meter Sci, 14(1): 209-213.
[46]岳彩军, 寿亦萱, 寿绍文, 等.2008.各非地转<i><b>Q</b></i>矢量之间的定量比较[J].高原气象, 27(3): 608-618.
[47]Yue Caijun, Shou Yixuan, Shou Shaowen, et al.2008.The quantitative comparisons among ageostrophic <i><b>Q</b></i>-vectors[J].Plateau Meteor, 27(3): 608-618.