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| 东亚夏季风的自然变率——NCARCam3模拟结果分析 | |
| 引用本文： | 曾刚,孙照渤,林朝晖,朱艳峰,李春晖.东亚夏季风的自然变率——NCARCam3模拟结果分析[J].南京气象学院学报,2009,32(4):498-506. |
| 作者姓名： | 曾刚 孙照渤 林朝晖 朱艳峰 李春晖 |
| 作者单位： | 1. 南京信息工程大学气象灾害省部共建教育部重点实验室,江苏,南京,210044;中国气象局气候研究开放实验室,北京,100081 2. 南京信息工程大学气象灾害省部共建教育部重点实验室,江苏,南京,210044 3. 中国科学院大气物理研究所国际气候和环境科学中心,北京,100029 4. 中国气象局气候研究开放实验室,北京,100081 5. 中国气象局广州热带海洋气象研究所,广东,广州,510080 |
| 基金项目： | 中国气象局气候研究开放实验室开放课题，广州热带海洋气象研究所热带海洋科学基金项目，江苏省高校自然科学摹础研究面上项目，中国科学院知识创新工程领域前沿项目，江苏省"六大人才高峰"计划资助项目 |
| 摘 要： | 利用季节循环的全球观测海表温度及海冰驱动NCARCam3全球大气环流模式的100a模拟结果，通过定义东亚夏季风指数，分析了模拟的大气内部变化中东亚夏季风的变化特征。结果表明：模拟的东亚夏季风自然变率主要表现为3—7a较显著的年际周期，并具有较明显的年代际变化特征。在弱夏季风年代，亚洲大陆海平面气压增强，日本附近及东亚沿海地区海平面气压降低；500hPa位势高度上，欧洲地区为负高度距平，里海附近地区为正高度距平，日本及其以东太平洋为负高度距平，易形成类似欧亚（EU）型的遥相关波列。在强夏季风年代，其环流异常分布基本与弱夏季风年代相反。模拟的东亚夏季风变化与夏季大气内部500hPa高度场上EU型遥相关波列的关系密切。 |
| 关 键 词： | 东亚夏季风 自然变率 数值模拟 年代际变化 |
Natural Variability of East Asian Summer Monsoon:Analysis of NCAR Cam3 Model Simulations |
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| ZENG Gang,SUN Zhao-bo,LIN Zhao-hui,ZHU Yan-feng,LI Chun-hui.Natural Variability of East Asian Summer Monsoon:Analysis of NCAR Cam3 Model Simulations[J].Journal of Nanjing Institute of Meteorology,2009,32(4):498-506. | |
| Authors: | ZENG Gang SUN Zhao-bo LIN Zhao-hui ZHU Yan-feng LI Chun-hui |
| Institution: | ZENG Gang, SUN Zhao-bo , LIN Zhao-hui, ZHU Yan-feng, LI Chun-hui( ( 1. Key Laboratory of Meteorological Disaster of Ministry of Education,NUIST,Nanjing 210044 ,China; 2. Laboratory for Climate Studies,China Meteorological Administration, Beijing 100081, China; 3. International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences,Beijing 100029,China; 4. Guangzhou Institute of Tropical Marine Meteorology, China Meteorological Administration,Guangzhou 510080,China) |
| Abstract: | Using the 100-yr simulations from seasonal cycle global SST and sea ice-driven NCAR Cam3 global atmospheric circulation model, the variation of simulated East Asian Summer Monsoon (EASM) in the model atmosphere is investigated with an EASM index. Results suggest that the natural variability of the simulated EASM mainly displays 3--7-yr period and marked interdecadal variation. During the weak EASM period, the sea level pressure (SLP) over the Asian continent increases, with decreased SLP around Japan and eastern Asian littoral;the 500 hPa geopotential height fields exhibit the negative height anomaly over the Europe, the positive anomaly around the Caspian Sea, and the negative anoma-ly around Japan and the Pacific area east of Japan, thus forming an Eurasian (EU)-like teleconnection wavetrain;and almost v. v. during the strong EASM period. It is also found that the simulated EASM variation has a close relation to the EU teleconnection wavetrain at 500 hPa in summer. |
| Keywords: | East Asian summer monsoon natural variability numerical simulation interdecadal variation |
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