近10年廣東冰雹的統(tǒng)計特征及天氣形勢
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華南區(qū)域氣象中心科技攻關(guān)項(xiàng)目(GRMC2012M01)、廣東省氣象局科技研究項(xiàng)目(2013B26)、公益性行業(yè)(氣象)科研專項(xiàng)項(xiàng)目(GYHY201406009)、華南區(qū)域氣象中心科技攻關(guān)項(xiàng)目(GRMC2012M06)共同資助


Statistical Characteristics and Circulation Patterns of Hails in Guangdong in Recent 10 Years
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    摘要:

    對2004—2013年廣東冰雹天氣的時空分布、天氣形勢、物理量進(jìn)行了分析。廣東的冰雹天氣主要出現(xiàn)在3—5月并且集中在粵北山區(qū)和西江流域河網(wǎng)地帶。可將廣東出現(xiàn)冰雹時的天氣形勢分成鋒面低槽型、暖區(qū)型、高架雷暴型3種典型的類型。鋒面低槽型,大冰雹多出現(xiàn)在這類天氣形勢下,地面冷鋒、低層切變線(低渦)、高空槽(溫度槽)互相配合,地面冷空氣和中層溫度槽的侵入,使得大氣層結(jié)變的不穩(wěn)定;鋒面、切變線、高空槽的動力作用觸發(fā)對流;冰雹出現(xiàn)在鋒面、切變線附近,高空槽前。暖區(qū)型,地面在長江流域以南沒有冷空氣活動,低層存在西南風(fēng)與東南風(fēng)的輻合,高空槽帶來干冷空疊加在低層暖濕氣流之上,形成不穩(wěn)定層結(jié);冰雹出現(xiàn)在高空槽前、低層輻合區(qū)內(nèi)。高架雷暴型,地面為冷高壓控制,低空存在逆溫層,暖濕氣流沿著低層冷墊爬升,對流在逆溫層之上發(fā)展;冰雹出現(xiàn)在切變線附近,多為小冰雹。在廣東,適宜大冰雹生長的物理量平均值是:0 ℃層高度4505 m,-20 ℃層高度7632 m,K指數(shù)35 ℃,SI指數(shù)-099 ℃;垂直風(fēng)切變267×10-3 s-1;最大上升速度-28×10-2 Pa/s,400 hPa與700 hPa之間的差動溫度平流-239×10-5 ℃/s。大冰雹要求更大的K指數(shù)、更小的SI、更大的垂直風(fēng)切變、更加充足的水汽、更加強(qiáng)烈的垂直上升速度、更大的差動溫度平流。

    Abstract:

    The temporal and spatial distributions, circulation patterns and physical quantities of hails in Guangdong in Recent 10 years are analyzed. In Guangdong, hail weather occurs mostly in March, April and May, and hails occurred more frequently in the northern Guangdong and the Xijiang River region. The typical circulation patterns of hails can be divided into three types: cold front with trough (typeⅠ), warm zoon (typeⅡ), and elevated thunderstorms (type Ⅲ). Most severe hails happened in typeⅠ; that is,the cold front accompanies with the lowlevel shear line (vortex) and upper trough (temperature trough), and the surface cold air and the intrusion of temperature trough at upper levels make the atmosphere unstable. Severe convective weather is driven by the cold front, shear line, and trough, and the locations of hails in typeⅠare usually in front of the upperlevel trough, near the cold front and shear line. In typeⅡ, there is no cold front to the south of the Yangtze River on surface, and there is a convergence region of southeasterly and southerly at low levels over Guangdong. The drycold air brought by the upperlevel trough overlaps over the warmmoist air, leading to unstable stratification. The locations of hails in typeⅡare usually in the convergence region in front of the trough. In type Ⅲ, Guangdong is behind a cold front, and there is a lowlevel temperature inversion, and warm and moist air lifting convectively above the temperature inversion. The locations of hails in type Ⅲ are often near the shear line and hails are generally small.The mean environmental physical quantities favorable for severe hails are: the height of 0 ℃ is 4505 m; the height of -20 ℃ is 7632 m; Kindex is 35 ℃; SIindex is -099 ℃; the vertical wind shear is 267×10-3 s-1; the pressure vertical velocity is -28×10-2Pa/s; differential temperature advection between 400 hPa and 700 hPa is -239×10-5℃/s. Severe hails require larger Kindex, vertical wind shear, vertical velocity, differential temperature advection, more water vapor supply and smaller SIindex.

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李懷宇,何如意,胡勝,張羽,羅聰.近10年廣東冰雹的統(tǒng)計特征及天氣形勢[J].氣象科技,2015,43(2):261~269

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  • 收稿日期:2014-04-17
  • 最后修改日期:2014-08-11
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  • 在線發(fā)布日期: 2015-04-28
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