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中国华北雾霾天气与超强El Ni?o事件的相关性研究
引用本文:袁媛,周宁芳,李崇银.中国华北雾霾天气与超强El Ni?o事件的相关性研究[J].地球物理学报,2017,60(1):11-21.
作者姓名:袁媛  周宁芳  李崇银
作者单位:1. 国家气候中心, 中国气象局气候研究开放实验室, 北京 100081;2. 国家气象中心, 北京 100081;3. 中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室, 北京 100029;4. 解放军理工大学气象海洋学院, 南京 211101
基金项目:国家重点基础研究发展计划(973)项目(2013CB956203,2013CB430203)、国家自然科学基金项目(41490642,41575090)、中国气象局预报预测核心业务发展专项(CMAHX20160401)和公益性气象行业专项(GYHY200906016)共同资助.
摘    要:2015年11—12月,全国接连发生七次大范围、持续性雾霾天气过程,其中,11月27日—12月1日的雾霾天气过程持续时间长达五天,成为2015年最强的一次重污染天气过程;12月19-25日重度雾霾再次发展,影响面积一度达到35.2万km~2.本文利用多种数据资料通过个例对比和历史统计详细分析了超强El Ni?o背景下雾霾天气频发的天气气候条件.其结果清楚表明:2015年11—12月欧亚中高纬度以纬向环流为主,东亚冬季风偏弱,使得影响我国的冷空气活动偏少,我国中东部大部地区对流层低层盛行异常偏南风,大气相对湿度明显偏大,并且大气层结稳定,对流层底层存在明显逆温.上述大气环流条件使得污染物的水平和垂直扩散条件差,因此在有一定污染排放的情况下,造成了重度雾霾天气过程的频发.由此,超强El Ni?o事件所导致的大尺度大气环流异常是我国中东部,尤其华北地区冬季雾霾天气频发的重要原因之一.

关 键 词:超强El  Niñ  o  中国华北  雾霾  冬季风  大气稳定度  逆温  
收稿时间:2016-03-06

Correlation between haze in North China and super El Niño events
YUAN Yuan,ZHOU Ning-Fang,LI Chong-Yin.Correlation between haze in North China and super El Niño events[J].Chinese Journal of Geophysics,2017,60(1):11-21.
Authors:YUAN Yuan  ZHOU Ning-Fang  LI Chong-Yin
Institution:1. National Climate Center, Laboratory for Climate Studies, China Meteorological Administration, Beijing 100081, China;2. National Meteorological Center, China Meteorological Administration, Beijing 100081, China;3. LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;4. Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101, China
Abstract:During November-December 2015, seven strong fog and haze events persistently occurred over a large area of eastern China. Of them, the most severe one was from 27 November to 1 December, which lasted for five days or more. The second one was from 19 to 25 December 2015, which covered a large area up to 352000 square kilometers. Using multiple datasets, this study analyzes meteorological and climate conditions for these fog and haze events. The results clearly show that anomalous 500 hPa zonal circulation dominated over mid-high latitudes of Eurasia during November to December 2015, with weak East Asian winter monsoon, weaker cold air activities, and anomalous low-level southerlies over most areas of eastern China. Meanwhile, the relative humidity over eastern China was larger than normal, and the anomalous inversion in near-surface increased the stability of the surface air. The above atmospheric circulation conditions were unfavorable for horizontal and vertical diffusion of pollutants. As a result, severe fog and haze events occur frequently under the circumstance of pollutant emissions. Therefore, the large-scale atmospheric circulation anomalies caused by super El Niño events should be one of the most important reasons for these fog and haze disasters in eastern China, especially in North China.
Keywords:Super El Niño  North China  Fog and haze  Winter monsoon  Atmospheric stability  Inversion
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