中国近海温带气旋的时空变化特征

秦听; 魏立新

doi:10.3969/j.issn.0253-4193.2015.01.005

中国近海温带气旋的时空变化特征

doi: 10.3969/j.issn.0253-4193.2015.01.005

秦听,
魏立新

国家海洋局海洋灾害预报技术研究重点实验室, 北京 100081;国家海洋环境预报中心, 北京 100081

基金项目: 国家自然科学基金青年基金项目(41206186);海洋国际合作及履约《中国-美国南大洋气旋演变特征及海气通量在其演变过程中的作用》;极地专项《南极周边海域气象环境综合分析与评价》(CHINAER 2013-04-01);极地专项《北极地区环境与资源潜力综合评估》(CHINARE 2014-04-03)。

计量
- 文章访问数: 1454
- HTML全文浏览量: 16
- PDF下载量: 1385
- 被引次数: 0
出版历程
- 收稿日期: 2013-07-17
- 修回日期: 2014-11-09

The statistic and variance of cyclones entering coastal waters of China in 1979-2012

Qin Ting,
Wei Lixin

Key Laboratory of Marine Environmental Information Technology, State Oceanic Administration, Beijing 100081, China;National Marine Environmental Forecasting Center, Beijing 100081, China

摘要

摘要: 基于1979-2012年共34年的ECMWF逐日4次平均海平面气压的再分析资料,采用英国雷丁大学气旋客观追踪算法,对出现在我国近海的温带气旋(气旋生命史1 d以上,移动距离大于500 km)的时空分布特征进行统计分析。结论包括以下几点:(1)1979-2012年进入中国近海的温带气旋平均每年45个,气旋数量呈现春夏多而秋冬少的特点。20世纪90年代初至今,气旋数量呈增加趋势,其中北部海区气旋数量增加达到显著水平,东部海区气旋数量表现为不显著减少,故认为影响中国近海的气旋路径有北移的趋势。(2)进入我国近海的温带气旋主要有4个生成源地,按比例由高到低分别是江淮气旋(38.9%),东海气旋(25.2%),黄河气旋(24.3%)以及蒙古气旋(11.6%)。气旋入海后,当大气海洋条件适合时,可以爆发性增长,气旋爆发性增长的主要区域在朝鲜半岛及以东洋面以及日本以东洋面,在我国近海气旋爆发的比例较小。(3)气旋生命史主要为1~7 d,但生命史为1~4 d的气旋比例最大,平均占气旋总数的52%,其中夏季长生命史气旋(大于10 d)的比例最大,为8%,冬季最少,接近3%。冬季气旋最强,气压分布区间大;夏季弱气旋多,中心气压分布集中。
- 中国近海 /
- 温带气旋 /
- 自动气旋追踪 /
- 时空分布 /
- 爆发性气旋
Abstract: Based on the 6 hourly sea level pressure data of ERA-Interim reanalysis over the period 1979-2012 and automated cyclone detection and tracking algorithm from Reading University,extratropical cyclones entering coastal waters of China are examined and their activities such as source,distribution,intensity,frequency,life time,annual and seasonal variability and so on are investigated. Conclusions are as follows:(1)From 1979 to 2012,there are 1 530 extratropical cyclones are detected in coastal waters of China,45 per year on average. Since the early 1990s the number of extratropical cyclone in coastal waters of China shows positive trend,and the route has a tendency to move northward. This is consistent with previous research conclusion of extratropical cyclone in the northern hemisphere. Especially in the north of coastal waters of China ,cyclone number increased significantly. (2)These cyclones mainly come from four regions,Jianghuai,Yellow River,East China Sea and Mongolia,and the most proportion is Jianghuai,the least is Mongolia,especially in summer. When atmospheric and ocean conditions meet the requirements,the cyclones can growth explosively.The main sources of explosive cyclones are east ocean of Japan and the east ocean of of Korean Peninsula,compare to this tow place,there are less cyclones can growth explosively in coastal waters of China .The number of explosive cyclones is the largest in spring,the least in summer. More than half of the cyclone's life is for 1 to 4 days,the number of long life cyclones(more than 10 days) is the largest in summer,the least in winter. The cyclones are more stronger in winter and more weaker in summer.
- coastal waters of China /
- automated cyclone detection and tracking algorithm /
- extratropical cyclones /
- explosive cyclones /
- temporal and spatial distribution

HTML全文

参考文献(21)

朱乾根,林锦瑞,寿绍文.天气学原理和方法[M].北京:气象出版社,2000:122-123. Zhu Qiangen, Lin Jinrui, Shou Shaowen. Principles of Synoptic Meteorology[M]. Beijing: China Meteorological Press,2000:122-123.

Akyildiz V. Systematic errors in the behavior of cyclones in the ECMWF operational models[J]. Tellus. 1984,37(A): 297-308.

Murray R J,Simmonds I. A numerical scheme for tracking cyclone centers from digital data. Part I: Development and operation of the scheme[J]. Australian Meteorological Mag,1991,39: 155-166.

Hodges K I. A general method for tracking analysis and its application to meteorological data[J]. Monthly Weather Review,1994,122:2573-2586.

Gulev S K,Zolina O,Grigoriev S. Extratropical cyclone variability in the Northern Hemisphere winter from the NCEP/NCAR reanalysis data[J]. Climate Dynamics,2001,17: 795-809.

Zhang X,Walsh J,Zhang J,et al. Climatology and interannual variability of Arctic cyclone activity,1948-2002[J]. Climate,2004,17:2300-2317.

Sorteberg A,Walsh J E. Seasonal cyclone variability at 70°N and its impact on moisture transport into the Arctic[J]. Tellus,2008,60(A):570-586.

Uotila P T,Vihma T A,Pezza I,et al. Relationships between Antarctic cyclones and surface conditions as derived from high-resolution numerical weather prediction data[J]. Journal of Geophysical Research,2011,116:D07109.

David A J,Simmonds I. A climatology of Southern Hemishere extratropical cyclones[J]. Climate Dynamics,1993,9:131-145.

吴伯雄,刘长盛.东亚气旋活动的统计研究[J].南京大学学报:自然科学版,1958,2:1-22. Wu Boxiong, Liu Changsheng. The statistical investigation of the activity of extratropical cyclones in east asia[J]. Journal of Nanjing University(Natural Sciences),1958,2:1-22.

王荣华.东亚温带低压路径[J].气象学报,1963,1:17-23. Wang Ronghua. The tracks of the extratropical cyclones in eastern asia[J]. Acta Meteorologica Sinica(in Chinese), 1963,1:17-23.

王艳玲.近50a东亚-西太平洋温带气旋活动的气候特征及异常分析[D].南京:南京信息工程大学,2005. Wang Yanling. Climate characteristics of extratropical cyclone activity and its anomaly over East Asia and West Pacific during recent 50 years[D]. Nanjin:Nanjin University of Information Science and Technology, 2005.

齐桂英.北太平洋爆发型气旋的气候特征[J].应用气象学报,1993,4:426-433. Qi Guiying. Climatic characteristics of explosive cyclone over the North Pacific ocean[J]. Journal of Applied Meteorological Science, 1993,4:426-433.

秦臻灏,李永平,黄立文.中国近海和西太平洋温带气旋的气候学研究[J].海洋学报,2002,3:105-111. Qin Zenghao, Li Yongping, Huang Liwen. Climatology of the extratropical cyclones over the East China sea and the West Pacific[J]. Haiyang Xuebao, 2002,3:105-111.

董立清,李德辉.中国东部的爆发性海岸气旋[J].气象学报,1989,3:373-375. Dong Liqing, Li Dehui. Coastal and oceanic explosive cyclones to the East of China[J]. Acta Meteorologica Sinica (in Chinese), 1989,3:373-375.

Hodges K I. Feature tracking on the unit sphere[J]. Monthly Weather Review,1995,123:3458-3465.

Hodges K I. Spherical nonparametric estimators applied to the UGAMP model integration for AMIP[J]. Monthly Weather Review,1996,124: 2914-2932.

Sanders F,Gyakum J R. Synoptic-dynamic climatology of the‘bomb’[J]. Monthly Weather Review,1980,108: 1589-1606.

齐桂英.爆发性温带气旋的定义标准初探[J].海洋学报,1993,15(3):133-139. Qi Guiying. The definition standard of explosive extratropical cyclone[J]. Haiyang Xuebao, 1993,15(3):133-139.

丁一汇.高等天气学[M].北京:气象出版社,2005:174-187. Ding Yihui. Advanced synoptic meteorology[M]. Beijing:China Meteorological Press, 2005:174-187.

张颖娴,丁一汇,张巧萍.北半球温带气旋活动和风暴路径的年代际变化[J].大气科学,2012,36(5):913-928. Zhang Yingxian, Ding Yihui, Li Qiaoping. Interdecadal variations of extratropical cyclone activities and storm tracks in the Northern hemisphere[J]. Chinese Journal of Atmospheric Sciences (in Chinese), 2012,36(5):913-928.

施引文献

资源附件(0)

访问统计