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投稿时间:2015-04-24 修订日期:2015-06-15
投稿时间:2015-04-24 修订日期:2015-06-15
中文摘要: 根据1981—2013年浙江省地面气象观测资料对浙江省冬季霾的时空分布特征进行分析发现,20世纪80年代中期起冬季霾呈显著上升趋势;空间分布总体特征表现为北多南少、西多东少,盆地平原多、丘陵岛屿少。利用K 均值聚类法将近33年冬季的主要霾过程分为盆地 平原型和全省型两类,其中超过62%的个例表现为盆地平原型,该型以12月发生比例最高;全省型霾过程在12和1月均多发。从气流输送及冷空气强度、垂直运动和干区分布等大气环流背景条件方面对比两类霾过程的形成机理差异发现:盆地 平原型冬季霾多在北方冷空气南下,浙江省受较强冷高压和下沉气流控制时形成,气流来自高纬度;全省型冬季霾则在变性减弱的冷高控制下,下沉气流较弱、不利本地污染源扩散的情况下发生。
中文关键词: 冬季霾, 气候特征, K 均值聚类, 后向气流轨迹
Abstract:Based on available observation data of Zhejiang Province for the period from 1981 to 2013, temporal and spatial distribution characteristics of winter haze in Zhejiang Province were analyzed. The results show that haze days have increased significantly since the mid 1980s. Haze days in the northern and western part of the province are much more than the south and the east, also more in the basin and plain than on the hills and islands. The division of the haze distribution pattern is obtained according to the K means clustering analysis, which shows the pattern can be divided into two categories. The first category accounts for 62% of the total haze, most of which happens in December, while most of the second category usually appears in January and December. In the end, according to the NCEP/NCAR reanalysis data, the different atmospheric circulation features, including the strength of cold high, vertical velocity and the distribution of water vapor, are discussed for the two kinds of haze patterns respectively. It is found that Zhejiang Province is controlled by cold high from northern China and the sinking airflow in the first haze pattern. In the second haze pattern, however, the cold high has transformed, and the sinking flow is also weakened, which makes air move slowly, so it is hard for pollutants to dissipate.
文章编号: 中图分类号: 文献标志码:
基金项目:台州市社会发展科技项目(14SF01)和国家重点基础研究发展计划(973计划)(2015CB453200)共同资助
作者 | 单位 |
翁之梅 | 南京信息工程大学大气科学系, 南京 210044 台州市气象局, 台州 318000 |
李丽平 | 南京信息工程大学大气科学系, 南京 210044 |
杨万裕 | 台州市气象局, 台州 318000 |
刘力源 | 台州市气象局, 台州 318000 |
引用文本:
翁之梅,李丽平,杨万裕,刘力源,2016.浙江省冬季不同霾过程的后向气流轨迹及环流特征[J].气象,42(2):183-191.
WENG Zhimei,LI Liping,YANG Wanyu,LIU Liyuan,2016.Backward Trajectory and Circulation Features in Different Haze Processes in Winter of Zhejiang[J].Meteor Mon,42(2):183-191.
翁之梅,李丽平,杨万裕,刘力源,2016.浙江省冬季不同霾过程的后向气流轨迹及环流特征[J].气象,42(2):183-191.
WENG Zhimei,LI Liping,YANG Wanyu,LIU Liyuan,2016.Backward Trajectory and Circulation Features in Different Haze Processes in Winter of Zhejiang[J].Meteor Mon,42(2):183-191.