Page 114 - 《高原气象》2026年第2期
P. 114

高     原      气     象                                 45 卷
              414
                 Li Y, Li J Q, et al, 2022. Study of a heavy rainfall weather in   模型的建立[J]. 气象研究与应用, 40(3): 38-42. Min T, Wu
                 Ya’an  under  the  influence  of  850  hpa  low-level  jet[J]. Plateau   Y P, Wu X, et al, 2019. Characteristics of rainstorm in Ya’an re‐
                 and Mountain Meteorology Research, 42(1): 19-23. DOI: 10.  gional  warm  zone  and  its  conceptual  model  establishment[J].
                 3969/j. issn. 1674-2184. 2022. Z1. 004.           Journal  of  Meteorological  Research  and  Application,  40(3):
             江叶, 刘艳霞, 文军, 等, 2024. 一次典型西南涡降水的垂直结构和                 38-42.
                 微物理特征研究[J]. 成都信息工程大学学报, 39(6): 718-            彭贵康, 柴复新, 曾庆存, 等, 1994.“雅安天漏”研究 Ⅰ: 天气分析
                 726. DOI: 10. 16836/j. cnki. jcuit. 2024. 06. 011. Jiang Y, Liu Y   [J]. 大气科学, 18(4): 466-475. Peng G K, Chai F X, Zeng Q
                 X, Wen J, et al, 2024. Vertical structure and microphysical char‐  C, et al, 1994. Research on “Ya-An-Tian-Lou”, Part Ⅰ: weath‐
                 acteristics of clouds and precipitation induced by a typical south‐  er analysis[J]. Scientia Atmospherica Sinica, 18(4): 466-475.
                 west  vortex[J]. Journal  of  Chengdu  University  of  Information   王喆, 王振会, 曹晓钟, 2016. 毫米波雷达与无线电探空对云垂直结
                 Technology,  39(6):  718-726. DOI:  10. 16836/j. cnki. jcuit.  构探测的一致性分析[J]. 气象学报, 74(5): 815-826. DOI: 10.
                 2024. 06. 011.                                    11676/qxxb2016. 057. Wang Z, Wang Z H, Cao X Z, et al, 2016.
             金祺, 袁野, 刘慧娟, 等, 2015. 江淮之间夏季雨滴谱特征分析[J]. 气             Consistency analysis for cloud vertical structure derived from mil‐
                 象学报, 73(4): 778-788. DOI: 10. 11676/qxxb2015. 036. Jin Q,   limeter cloud radar and radiosonde profiles[J]. Acta Meteorologi‐
                 Yuan Y, Liu H J, et al, 2015. Analysis of microphysical character‐  ca Sinica, 74(5): 815-826. DOI: 10. 11676/qxxb2016. 057.
                 istics of the raindrop spectrum over the area between the Yangtze   徐裕华, 1991. 西南气候[M]. 北京: 气象出版社, 298. Xu Y H,
                 River and the Huaihe River during summer[J]. Acta Meteorologi‐  1991. Climate of Southwest China[M]. Beijing: China Meteoro‐
                 ca Sinica, 73(4): 778-788. DOI: 10. 11676/qxxb2015. 036.  logical Press, 298.
             刘黎平, 郑佳锋, 阮征, 等, 2015. 2014年青藏高原云和降水多种雷            杨康权, 肖递祥, 罗辉, 等, 2019. 四川盆地西部两次暖区暴雨过程
                 达综合观测试验及云特征初步分析结果[J]. 气象学报, 73                    分析[J]. 气象科技, 47(5): 795-808. DOI: 10. 19517/j. 1671-
                (4): 635-647. DOI: 10. 11676/qxxb2015. 041. Liu L P, Zheng J   6345. 20180405. Yang  K  Q,  Xiao  D  X,  Luo  H,  et  al,  2019.
                 F,  Ruan  Z,  et  al,  2015. The  preliminary  analyses  of  the  cloud   Analysis of two warm-sector heavy rain processes in western Si‐
                 properties over the Tibetan Plateau from the field experiments in   chuan  Basin[J]. Meteorological  Science  and  Technology,  47
                 clouds precipitation with the various radars[J]. Acta Meteorologi‐  (5): 795-808. DOI: 10. 19517/j. 1671-6345. 20180405.
                 ca Sinica, 73(4): 635-647. DOI: 10. 11676/qxxb2015. 041.  张琪, 李跃清, 陈权亮, 等, 2011. 近 46 年西南地区云量的时空变
             罗晶, 2023. 基于星载测雨雷达观测对夏季青藏高原降水特征的研                     化 特 征[J]. 高 原 气 象 , 30(2): 339-348. Zhang Q, Li Y Q,
                 究[D]. 合肥: 中国科学技术大学 . Luo J, 2023. A study of sum‐  Chen  Q  L,  et  al,  2011. Temporal  and  spatial  distributions  of
                 mer precipitation characteristics on the Tibetan Plateau based on   cloud cover over southwest China in recent 46 years[J]. Plateau
                 satellite-borne  precipitation  radar  observations[D]. Hefei:  Uni‐  Meteorology, 30(2): 339-348.
                 versity of Science and Technology of China.    郑佳锋, 2016. Ka波段—多模式毫米波雷达功率谱数据处理方法及
             梅双丽, 陈尚锋, 2022. 华西秋雨变异特征及其成因分析[J]. 高原气                云内大气垂直速度反演研究[D]. 南京: 南京信息工程大学.
                 象, 41(6): 1492-1500. DOI: 10. 7522/j. issn. 1000-0534. 2021.  Zheng J F, 2016. Doppler spectral data processing methods of Ka-
                 00092. Mei S L, Chen S F, 2022. Varation characteristics causes   band multi-mode mm-wave Radar and air vertical speed retrieval
                 of autumn rain in western China[J]. Plateau Meteorology, 41(6):   in clouds[D]. Nanjing: University of Information Technology.
                 1492-1500. DOI: 10. 7522/j. issn. 1000-0534. 2021. 00092.  周秋雪, 李跃清, 蒋兴文, 等, 2016.“雅安天漏”降水变化气候特征
             苗秋菊, 徐祥德, 施小英, 2004. 青藏高原周边异常多雨中心及其                   的分析[J]. 自然资源学报, 31(2): 343-353. DOI: 10. 11849/
                 水汽输送通道[J]. 气象, 30(12): 44-47. Miao Q J, Xu X D,   zrzyxb. 20141350. Zhou Q X, Li Y Q, Jiang X W, et al, 2016.
                 Shi  X  Y,  2004. Water  vapor  transport  structure  of  anomalous   Analysis on the climatic characteristics of the precipitation varia‐
                 rainy centers in the ambient area of Tibetan Plateau[J]. Meteoro‐  tions at “Ya’an Sky-leakage”[J]. Journal of Natural Resources,
                 logical Monthly, 30(12): 44-47.                   31(2): 343-353. DOI: 10. 11849/zrzyxb. 20141350.
             闵涛, 吴筱, 高文良, 等, 2020. 雅安市一次暖区强降水过程中多普              竹利, 蒋兴文, 卢萍, 等, 2024. 雅安地区一次暖区暴雨过程的对流
                 勒雷达回波特征分析[J]. 中低纬山地气象, 44(3): 13-18.              触发机制分析[J]. 大气科学, 48(5): 1693−1710. DOI: 10.
                 Min T, Wu X, Gao W L, et al, 2020. Analysis of Doppler radar   3878/j. issn. 1006-9895. 2311. 23074. Zhu L, Jiang X W, Lu P,
                 echo  characteristics  in  a  warm-sector  heavy  rainfall  process  in   et al, 2024. Analysis of the convective triggering mechanism of a
                 Ya’an[J]. Mid-low  Latitude  Mountain  Meteorology,  44(3):   warm-sector rainstorm in the Ya’an region[J]. Chinese Journal of
                 13-18.                                            Atmospheric  Sciences,  48(5):  1693 − 1710. DOI:  10. 3878/j.
             闵涛, 吴亚平, 吴筱, 等, 2019. 雅安区域性暖区暴雨特征及其概念                 issn. 1006-9895. 2311. 23074.
   109   110   111   112   113   114   115   116   117   118   119