Advanced Search
XING Caiying, KE Zongjian, WU Shengan, LIU Changzheng, DU Liangmin. 2016: Circulation characteristics of autumn rainstorm days anomaly and construction of its prediction model in Hainan. Torrential Rain and Disasters, 35(3): 203-209. DOI: 10.3969/j.issn.1004-9045.2016.03.002
Citation: XING Caiying, KE Zongjian, WU Shengan, LIU Changzheng, DU Liangmin. 2016: Circulation characteristics of autumn rainstorm days anomaly and construction of its prediction model in Hainan. Torrential Rain and Disasters, 35(3): 203-209. DOI: 10.3969/j.issn.1004-9045.2016.03.002

Circulation characteristics of autumn rainstorm days anomaly and construction of its prediction model in Hainan

More Information
  • Received Date: June 24, 2015
  • Accepted Date: March 24, 2016
  • Available Online: November 03, 2022
  • Published Date: June 14, 2016
  • By using daily precipitation at 18 meteorological automatic stations in Hainan, NCEP/NCAR monthly reanalysis data with a reso-lution of 2.5 °×2.5 °, NOAA SST and historical data of CFSv2 model, the corresponding atmospheric circulation characteristics of Hainan au-tumn rainstorm anomaly and its relationship to SST are analyzed for the period from 1982 to 2013. The circulation factors closely related to au-tumn rainstorm days, which are predicted well by CFSv2, and SST are extracted as predictors to build a predictive model of autumn rainstorm days. Results show the following. (1) Autumn rainstorm days in Hainan are closely related to atmospheric circulation. In more autumn rainstormyears, there is prevailing easterly wind near Hainan. Atmospheric pressure in the tropical western Pacific to south China sea is lower, the tropi-cal vortex systems tend to be more active, and there is a southeast wind anomaly in the region, which provides abundant moisture. The zonalwind shear in western Pacific is weaker, a warm core structure easily forms, corresponding to the occurrence and development of typhoon. On the other hand, the SST forcing effect is significant. In the context of the tropic central and eastern Pacific SST anomaly, atmospheric circula-tion and tropical convection activities are affected, resulting in autumn rainfall anomaly. (2) The autumn rainstorm days are closely associated with the lower level height field, sea level pressure, low level wind and zonal wind shear in the tropical Pacific. CFSv2 has good prediction skillon the high-impact areas of such circulation fields. (3) Predictive model of autumn rainstorm days is built by using optimal subset regression based on effective model information. The results of cross-validation and independent samples test demonstrate that the predictive method and model have good prediction skill, which can provide an effective reference for short-term climate prediction of autumn rainstorm days.

  • 赵付竹, 王凡, 郑艳".纳沙"、"尼格"强度和结构差异对海南暴雨分布的影响[J].广东气象, 2013, 35(2):14-20 doi: 10.3969/j.issn.1007-6190.2013.02.003
    杨仁勇, 闵锦忠, 郑艳.强台风"纳沙"引发的特大暴雨过程数值试验[J].高原气象, 2014, 33(3) : 753-761 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gyqx201403017
    刘丽君, 冯文, 陈德明.东风急流影响下海南非热带气旋暴雨个例分析[J].暴雨灾害, 2010, 29(4):328-333 doi: 10.3969/j.issn.1004-9045.2010.04.005
    马学款, 符娇兰, 曹殿斌.海南2008年秋季持续性暴雨过程的物理机制分析[J].气象, 2012, 38(7): 795-803 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK201203695357
    张维, 林少冰, 杜尧东, 等.华南地区1961—2008年暴雨事件的气候变化特征[J].气象与环境科学, 2011, 34(2): 20-24 doi: 10.3969/j.issn.1673-7148.2011.02.004
    杨仁勇, 赵付竹, 陈有龙. 2010年10月海南岛一次特大暴雨过程数值模拟和诊断分析[J].暴雨灾害, 2014, 33(3):255-263 doi: 10.3969/j.issn.1004-9045.2014.03.008
    汪汇洁, 孙建华, 赵思雄, 等.2010年秋季一次海南东海岸特大暴雨的中尺度分析[J].热带气象学报, 2014, 30(3): 518-532 doi: 10.3969/j.issn.1004-4965.2014.03.013
    李勇, 陆日宇, 何金海.海南岛秋季降水异常对应的热带大尺度环流和海温[J].大气科学, 2006, 30(5): 1 034-1 042 http://d.old.wanfangdata.com.cn/Periodical/daqikx200605029
    简茂球, 张春花.准双周振荡对2010年10月海南持续性暴雨的影响[J].热带气象学报, 2013, 29(3): 364-373 doi: 10.3969/j.issn.1004-4965.2013.03.002
    柯宗建, 张培群, 董文杰.最优子集回归方法在季节气候预测中的应用[J].大气科学, 2009, 33(5):994-1 002 doi: 10.3878/j.issn.1006-9895.2009.05.10
    顾伟宗, 陈丽娟, 张培群.基于月动力延伸预报最优信息的中国降水降尺度预测模型[J].气象学报, 2009, 67(2):280-287 doi: 10.3321/j.issn:0577-6619.2009.02.011
    刘颖, 范可, 张颖.基于CFS模式的中国站点夏季降水统计降尺度预测[J].大气科学, 2013, 37(6): 1 287-1 296 http://d.old.wanfangdata.com.cn/Periodical/daqikx201306011
    Zhao S, Yang S. Dynamical prediction of the early-season rainfall over southern China by the NCEP Climate Forecast System[J]. Wea Forecasting, 2014, 10: 1 391-1 401 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=7e8cb4caf92a335993ad85315c344c9e
    刘娜, 李双林.基于时间尺度分离的中国东部夏季降水预测[J].应用气象学报, 2015, 26(3): 328-337 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yyqxxb201503008
    Jia Xiaolong, Yang Song, Song Wenling, et al. Prediction of wintertime northern hemisphere blocking by the NCEP climate forecast system[J]. Journal of meteorological research, 2014, 28(1):76-90 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qxxb-e201401006
    李天然.华南冬半年降水对ENSO循环的不对称响应[D].北京: 中国气象科学研究院, 2013 http://cdmd.cnki.com.cn/Article/CDMD-85101-1013212445.htm
    刘长征, 杜良敏, 柯宗建, 等.国家气候中心多模式解释应用集成预测[J].应用气象学报, 2013, 24(6): 677-685 doi: 10.3969/j.issn.1001-7313.2013.06.004
    林美静, 范可, 王会军.西北太平洋区域纬向风垂直切变的气候特征研究[J].气象学报, 2010, 68(3): 309-314 doi: 10.3969/j.issn.1004-4965.2010.03.007
    庞昕, 吴洪宝.赤道低平流层纬向风垂直切变与ENSO变率的关系[J].南京气象学院学报, 2002, 25(1): 62-68 doi: 10.3969/j.issn.1674-7097.2002.01.008
    朱乾根, 林锦瑞, 寿绍文, 等.天气学原理和方法(第四版)[M].北京:气象出版社, 2000:541-550
    李崇银.厄·尼诺影响西太平洋台风活动的研究[J].气象学报, 1987, 45(2): 229-236 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000002438760
    何敏, 龚振淞, 徐明, 等.高低层纬向风异常与西北太平洋热带气旋生成年频数关系的研究[J].热带气象学报, 2007, 23(3): 277-283 doi: 10.3969/j.issn.1004-4965.2007.03.010
    陈官军, 魏凤英, 巩远发. NCEP_CFS模式对东亚夏季延伸预报的检验评估[J].应用气象学报, 2010, 21(6): 659-670 doi: 10.3969/j.issn.1001-7313.2010.06.003
    刘罗曼.用主成分回归分析解决回归模型中复共线性问题[J].沈阳师范大学学报(自然科学版), 2008, 26(1): 42-44 doi: 10.3969/j.issn.1673-5862.2008.01.012

Catalog

    Article views PDF downloads Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return