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投稿时间:2009-03-05
投稿时间:2009-03-05
中文摘要: 2008年,尽管总体来看,全国天气气候的持续异常较弱,未发生大范围持续干旱和严重洪涝
灾害,但依然出现了非常显著的天气气候异常特征,如全国平均年降水量比常年偏多,为近
10年来降水最多的年份;夏季华南降水异常偏多,黄淮降水偏多;年平均气温偏高,但冬季
气温偏低,年初南方遭遇罕见低温雨雪冰冻灾害;在南海和西太平洋生成的台风个数明显偏
少,但是登陆台风偏多,初台异常偏早。分析发现,2008年赤道中东太平洋总体处在冷水位
相,受海洋异常强迫和海气相互作用的影响,北半球大气环流表现出的主要特征是: 500hPa
西太平洋副高强度和位置变化较大; 冬夏季风均偏强; 冬春季西太平洋暖池区热带对流活
动偏强,夏秋季则偏弱;1月份,亚洲中高纬度经向环流异常发展,2至4月份则以纬向环流
为主,春季后期至秋季,经纬向环流的转换较快,环流的持续性较弱。这些环流异常是影响
2008 年中国气候异常的主要原因。
Abstract:Although overall in 2008, there are not serious persistent drought and flood d
isasters happened over countrywide due to the week anomalies of climate, some si
gnificant anomalies of synoptic and climatic features occurred in China such as
annual mean precipitation is above normal and ranked first among recent 10 years
,significant wet in South China and wet again in Huanghuai region during summe
r, annual mean temperature is above normal while cold in winter with rare snow s
torm and ice freeze disasters in south part of China in the beginning of the y
ear,significant less than normal of typhoon generated over South China Sea and West
Pacific. However, more than normal of typhoon landing China, as well as firs
t naming typhoon occurred very early than normal. It is shown by diagnostic anal
y
sis that below normal Sea Surface Temperature Anomalies (SSTa) are observed ove
r the central and eastern Pacific in 2008 followed a cold phase of ENSO occurred
in summer of 2007. Due to influence forced by SSTa and interaction between ocea
n and atmosphere, general circulation over the Northern Hemisphere shown the do
minant anomalies which have been characterized as respond as follows: the inten
sity and position of subtropical high over the West Pacific varied frequently th
an normal; East Asian monsoon was more strong than normal both in winter and sum
mer; the tropical convective activities in warm pool of West Pacific were more a
ctive from winter to spring and week from summer to fall of 2008 than normal; th
e meridional circulation develop strongly in January and the zonal circulation
develop strongly instead from February to April over mid high latitude area of
Asia, and the transition between meridional and zonal circulation was carried ou
t frequently from latter spring to fall indicated the week persistence of circul
ation. These may be the main factors that influence climate anomalies in China i
n 2008.
文章编号: 中图分类号: 文献标志码:
基金项目:
作者 | 单位 |
张培群 | 国家气候中心, 中国气象局气候研究开放实验室, 北京100081 |
贾小龙 | 国家气候中心, 中国气象局气候研究开放实验室, 北京100081 |
王永光 | 国家气候中心, 中国气象局气候研究开放实验室, 北京100081 |
引用文本:
张培群,贾小龙,王永光,2009.2008年海洋和大气环流异常及对中国气候的影响[J].气象,35(4):112-117.
Zhang Peiqun,Jia Xiaolong,Wang Yongguang,2009.Anomalies of Ocean and General Atmospheric Circulation in 2008 and Their Impacts on Climate Anomalies in China[J].Meteor Mon,35(4):112-117.
张培群,贾小龙,王永光,2009.2008年海洋和大气环流异常及对中国气候的影响[J].气象,35(4):112-117.
Zhang Peiqun,Jia Xiaolong,Wang Yongguang,2009.Anomalies of Ocean and General Atmospheric Circulation in 2008 and Their Impacts on Climate Anomalies in China[J].Meteor Mon,35(4):112-117.