| 登陆台风麦德姆不同部位降水强度及谱特征 |
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| 引用本文： | 林文,林长城,李白良,郑文君,胡伦善,余永江.登陆台风麦德姆不同部位降水强度及谱特征[J].应用气象学报,2016,27(2):239-248. |
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| 作者姓名： | 林文 林长城 李白良 郑文君 胡伦善 余永江 |
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| 作者单位： | 1.福建省气象科学研究所，福州 350001 |
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| 基金项目： | 资助项目： 公益性行业（气象）科研专项（GYHY201406033）,华东区域气象科技协同创新基金合作项目（QYHZ201406），中国气象局气象关键技术集成与应用项目（CMAGJ2015M46），福建省气象局开放式气象科学研究基金项目（2013K03） |
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| 摘 要： | 利用架设在福建省尤溪站和屏南站的两台PARSIVEL第2代激光雨滴谱仪对2014年7月23—25日影响福建省的台风麦德姆 (1410) 进行观测，尤溪站位于移动路径中轴，屏南站位于台风强降水的区域即右侧云系，观测显示了台风不同部位雨滴谱特征:台风麦德姆在外围右前侧和后侧以及残留云系出现强降水，台风中心为连续性降水，雨强变化平稳；台风右侧云系雨滴平均谱谱宽由宽变窄，小滴数浓度先增后减，大滴逐渐减少，移动路径中轴后侧的残留云系出现大滴数浓度和谱宽的突增；含水量与雨强变化一致, 雨强小于10 mm·h-1时，以大量的小粒子贡献为主，形状因子μ及斜率参数λ分布较广；雨强大于10 mm·h-1时，大滴的贡献随雨强增大而增大，μ及λ均减小；同时，可利用μ与λ线性函数关系对Gamma分布进行简化。
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| 关 键 词： | 雨滴谱 雨强 台风麦德姆 PARSIVEL |
| 收稿时间： | 2015-03-19 |
Rainfall Intensity and Raindrop Spectrum for Different Parts in Landing Typhoon Matmo |
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| Lin Wen,Lin Changcheng,Li Bailiang,Zheng Wenjun,Hu Lunshan and Yu Yongjiang.Rainfall Intensity and Raindrop Spectrum for Different Parts in Landing Typhoon Matmo[J].Quarterly Journal of Applied Meteorology,2016,27(2):239-248. |
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| Authors: | Lin Wen Lin Changcheng Li Bailiang Zheng Wenjun Hu Lunshan and Yu Yongjiang |
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| Institution: | 1.Fujian Institute of Meteorological Science, Fuzhou 3500012.Fujian Meteorological Observatory, Fuzhou 3500013.Youxi Meteorological Bureau of Fujian Province, Sanming 3651144.Pingnan Meteorological Bureauof Fujian Province, Ningde 352300 |
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| Abstract: | During typhoon Matmo passage over Fujian from 23 Jul to 25 Jul in 2014, it passes through two disdrometer sites: Pingnan and Youxi. Pingnan site locates in eastern Fujian that represents the heavy rain region of typhoon Matmo, and Youxi site represents the middle path region of typhoon Matmo moving. Thus, microphysical characteristics of raindrop size distribution in different parts of typhoon Matmo are studied through the PARSIVEL2 disdrometer measurements at these two sites. The evolution of raindrop size distribution parameters reveals different segments of the storm, that the fluctuation of rainfall intensity in the right part is stronger than those in the middle. Heavy rainfalls happen in right front side, rear side of outer rainband and residual cloud. There is showery in the outer rainband in which rainfall intensity fluctuate frequently. Approaching to the central region of typhoon Matmo, the precipitation becomes more continuous and rainfall intensity changes more smoothly. In the right side rainband, the spectral width of raindrop size distribution changes from wide to narrow, the concentration of small rain drops increases at first and then decreases, and concentration of large rain drops decreases gradually. In the middle path of typhoon Matmo, the concentration of small rain drops increases first and then decreases, but spectral width of raindrop size distribution and concentration of large rain drops suddenly rise for difference. The evaluation of raindrop concentration and liquate water has some certain relations to the changed rainfall intensity, but degrees of their changes are not in tune. When rainfall intensity is less than 10 mm·h-1, a large number of small droplets contribute to the precipitation. The contribution to rainfall intensity by large number of small raindrops is higher in the right side rainband than in the middle moving path. In the central region of typhoon Matmo, the contribution by high concentration of small raindrops to the rainfall intensity is higher than in front side and rear side rainband. On the contrary, when rainfall intensity is higher than 10 mm·h-1, the heavy rainfall in front outer rainband and residual cloud are the direct appearances by concentration growing of large droplets. The precipitation at Pingnan is more unstable than that at Youxi, so more fiercely collision broken processes lead to raindrop concentration repeating with droplets growing in right part of typhoon Matmo. Parameters of μ and λ meet the linear function both at 2 sites. Linear fit functions can be used to reduce Gamma distribution function, getting good results. The μ and λ have wide distributions in the region less than 10 mm·h-1. However, when rainfall intensity is more than 10 mm·h-1, parameters of μ and λ decrease with rainfall intensity increasing, and vary with rainfall intensity related to the region and precipitation types. |
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| Keywords: | raindrop size distribution rainfall intensity typhoon Matmo PARSIVEL |
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