| 珠江三角洲秋季大气边界层温度和风廓线观测研究 |
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| 引用本文： | 李明华,范绍佳,王宝民,吴兑,祝薇,刘吉,余冠明,鲍若峪,樊琦.珠江三角洲秋季大气边界层温度和风廓线观测研究[J].应用气象学报,2008,19(1):53-60. |
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| 作者姓名： | 李明华 范绍佳 王宝民 吴兑 祝薇 刘吉 余冠明 鲍若峪 樊琦 |
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| 作者单位： | 1.中山大学大气科学系/环境气象研究所, 广州 510275 |
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| 基金项目： | 国家自然科学基金
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国家重点基础研究发展计划(973计划) |
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| 摘 要： | 根据2004年10月珠江三角洲3个代表性观测点大气边界层观测资料, 分析了珠江三角洲秋季大气边界层温度和风廓线特征。结果表明:珠江三角洲秋季气温递减率较低, 逆温出现频率较高, 强度较弱, 海风使珠江口贴地逆温的出现时间推迟、低空逆温的出现频率增加。珠江三角洲秋季受多种局地环流影响, 边界层内风廓线比较复杂, 晚上城市群与非城市群地区风向有明显差别; 城市群和珠江口多次分别观测到城市热岛环流和海风环流。
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| 关 键 词： | 温度廓线 风廓线 珠江三角洲 秋季 |
| 收稿时间： | 2007-01-18 |
| 修稿时间： | 2007-10-15 |
Observation Study on the Temperature and Wind Profiles over the Pearl River Delta in Autumn |
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| Li Minghu,Fan Shaoji,Wang Baomin,Wu Dui,Zhu Wei,Liu Ji,Yu Guanming,Bao Ruoyu,Fan Qi.Observation Study on the Temperature and Wind Profiles over the Pearl River Delta in Autumn[J].Quarterly Journal of Applied Meteorology,2008,19(1):53-60. |
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| Authors: | Li Minghu Fan Shaoji Wang Baomin Wu Dui Zhu Wei Liu Ji Yu Guanming Bao Ruoyu Fan Qi |
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| Affiliation: | 1.Department of Atmospheric Sciences/Institute of Environmental Meteorology, Sun Yat-sen University, Guangzhou 5102752.Huizhou Meteorological Bureau, Huizhou 5160013.Institute of Tropical and Marine Meteorology, CMA, Guangzhou 5100804.Department of Environmental Sciences, Sun Yat-sen University, Guangzhou 510275 |
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| Abstract: | For the purpose of study on the characteristics of the boundary layer and its effects on air pollution in the Pearl River Delta, the comparison observation based on balloon sounding is conducted by Sun Yat-Sen University in Qingyuan, Panyu and Xinken of the Pearl River Delta in October, 2004. The temperature and wind profiles of the boundary layer over the Pearl River Delta in autumn are studied on the observation data.It is found that the temperature lapse rate is small while the occurrence frequency of the temperature inversion is high and the intensity is low over the Pearl River Delta in October, 2004. The surface temperature inversion occurs earlier over the city cluster than over the Pearl River estuary and the average intensity over the city cluster doubles that over the Pearl River estuary while the low-lever temperature inversion frequency over the city cluster is lower than that over the Pearl River estuary. The relatively low temperature and the high-speed sea breeze postpone the occurrence time of the surface temperature inversion and increase the occurrence frequency of the low-lever temperature inversion over the Pearl River estuary.It is also found that the Pearl River Delta is influenced by several kinds of local circulations and the wind profiles of the boundary layer are complex in October, 2004. The prevailing wind direction is northeast, and in the daytime the wind directions of the three sites are consistently in the northeast while in the nighttime there are obvious differences in wind direction between the city cluster and the non-city cluster, which is that the wind direction of the non-city cluster (Qinyuan and Xinken) is in the northeast and that of the city cluster is in the northwest. The city cluster is markedly characterized by local circulations and heat island circulation is frequently observed at night; the Pearl River estuary is markedly characterized by gradient wind and sea breeze circulation is frequently observed at night, and the occurrence frequency of 20-hour sea breeze is 51.8%; the local circulations of both the city cluster and the Pearl River estuary are observed under the same meteorological background of low-speed system wind and basically on the same dates. |
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| Keywords: | temperature profiles wind profiles the Pearl River Delta autumn |
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