| 再论夏季西太平洋副热带高压的西伸北跳 |
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| 引用本文： | 陶诗言, 卫捷. 再论夏季西太平洋副热带高压的西伸北跳. 应用气象学报, 2006, 17(5): 513-525. |
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| 作者姓名： | 陶诗言 卫捷 |
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| 作者单位： | 中国科学院大气物理研究所, 北京 100029 |
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| 基金项目： | 国家重点基础研究发展计划(973计划);中国科学院知识创新工程项目;中国科学院科技攻关项目 |
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| 摘 要： | 利用NCEP/NCAR再分析资料, 选择了1998年、2003年和2005年夏季我国东部雨带位置变化过程进行诊断分析。研究表明:夏季我国东部暴雨带位置的变动, 受西太平洋副热带高压西伸北跳 (南撤东退) 的调节。当副热带高压西伸北跳 (南撤东退) 时, 暴雨带向北 (向南) 移动。在副热带高压西伸北跳持续时期, 长江流域中下游地区出现高温酷暑天气。副热带高压西伸北跳是由于欧亚大陆上空存在静止Rossby波列, 波的能量沿着高空副热带急流向东传播到我国沿海海岸 (115°~130°E) 时, 在该地区激发出一个长波脊。这个长波脊的建立, 使得副热带高压和对流层上部的青藏高压都朝长波脊方向伸展, 表现为“相向”而行。而当在沿海海岸上空激发出一个长波槽时, 副热带高压南撤东退而青藏高压退回到高原上空。当夏季沿海海岸上空的长波脊持续维持时, 长江中下游会出现持久的高温酷暑天气。根据夏季天气预报的经验, 欧洲中期数值预报中心发布的预报对副热带高压的西伸北跳有较好的可预报性。
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| 关 键 词： | 副热带高压 西伸北跳 静止Rossby波列 下游效应 |
| 收稿时间： | 2006-04-10 |
| 修稿时间： | 2006-07-18 |
The Westward, Northward Advance of the Subtropical High over the West Pacific in Summer |
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| Tao Shiyan, Wei Jie. The westward, northward advance of the subtropical high over the west pacific in summer. J Appl Meteor Sci, 2006, 17(5): 513-525. |
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| Authors: | Tao Shiyan Wei Jie |
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| Affiliation: | Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 |
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| Abstract: | The subtropical high over the West Pacific in summer is one of the most important atmospheric circulation components which influences the weather and climate of China. Using the daily averaged data derived from NCEP/NCAR reanalysis dataset and interpolated outgoing longwave radiation (OLR) data provided by the National Oceanic and Atmospheric Administration (NOAA), the variation of the position of the summer rainfall belt in eastern China is diagnosed for the selected years of 2005, 2003 and 1998. The work analyzes the nonoccurrence of Meiyu in the mid and lower reaches of the Yangtze River during the summer of 2005, the heavy flood in the Yangtze River basin during the summer of 1998, as well as the prolonged heat wave south of the Yangtze River during the second half of July in 2003. Particular attention is devoted to the study on the correlation of these abnormal weather phenomena with the westward, northward advance or southward, eastward retreat of the subtropical high in the West Pacific.Evidence shows that the advance (retreat) of the subtropical high over the West Pacific in summer can modulate the positions of the heavy rainfall belt in eastern China. During the westward, northward advance (southward, eastward retreat) of the subtropical high, the heavy rainfall belt moves northward (southward). During the persistent advance of the subtropical high, a prolonged heat wave occurs in the mid and lower reaches of the Yangtze River. The process and mechanism of the westward, northward advance (southward, eastward retreat) of the subtropical high are revealed.Hoskins et al. show that the Asian Jet can act as a waveguide in the northern summer. Chang shows that the upper tropospheric waves over the mid-latitudes generally reveal the characteristics of downstream development in summer. Enomoto et al. study the relationship between the formation of the Bonin high in August and the energy propagation of stationary Rossby waves along the Asian Jet. Based on the results from previous studies, the work clearly demonstrates through the isentropic potential vorticity analyses that the advance (retreat) of the subtropical high is caused by the propagation of the stationary Rossby waves along the Asian Jet in the upper troposphere, forming a longwave ridge (trough) along the coast of China (115°—130°E); at the same time the subtropical high advances north westward (retreats southeastward). This anomalous ridge (trough) extends throughout the troposphere with the structure of the equivalent-barotropic ridge (trough). In summer when there is a persistent longwave ridge along the coast, there will be a prolonged heat wave in the mid and lower reaches of the Yangtze River.Based on the summer forecasting experiences, it is found that the medium range forecast issued by the ECMWF may better predict the westward, northward advance of the subtropical high of the West Pacific in summer. |
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| Keywords: | subtropical high the westward and northward advance stationary Rossby wave downstream effect |
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