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气象:2015,41(8):980-985
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0℃层高度的变化对冰雹融化影响的分析和应用
(1.大连市人工影响天气办公室,大连 116001;2.大连市气象服务中心,大连 116001;3.大连市气象台,大连 116001)
Analysis and Application of the Effect of 0℃ Layer Height on Melting Hail
(1.Dalian Weather Modification Office of Liaoning, Dalian 116001;2.Dalian Meteorological Service Centre of Liaoning, Dalian 116001;3.Dalian Meteorological Observatory of Liaoning, Dalian 116001)
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投稿时间:2014-03-27    修订日期:2015-03-07
中文摘要: 通过冰雹融化过程的热量平衡公式得到0℃层高度与冰雹融化能力的近似关系,分析小尺度冰雹条件下0℃层高度对0℃层冰雹半径和地面冰雹半径的影响。结果表明:地面冰雹半径随0℃层冰雹半径和0℃层高度变化,设定冰雹云判别的雷达回波高度和中心强度等指标时应考虑0℃层高度变化的影响;0℃层高度在2000~6000 m范围内时,0℃层冰雹最小半径临界值在0.32~1.08 cm,临界降雹的最小上升气流速度在11.5~21.2 m·s-1;结果分析可初步了解0℃层高度对冰雹融化的影响,为冰雹预报及人工防雹作业提供重要参考依据,降低通过WSR 88D增强HDA算法做冰雹尺寸预报的虚警率。
Abstract:Using thermal balance equation during the process of hail melting, the approximate relationship of 0℃ layer height (h0) and hail melting ability was obtained, and the influence of h0 to zero layer hail radius (r0) and ground hail radius (rg) was analyzed under the condition of small scale hail. The results show that rg changes with h0 and r0, so the hail cloud index setting such as radar echo height and center intensity is related to the change of h0, when h0 changes in the range of 2000-6000 m, the threshold of minimum zero layer hail radius changes between 0.32 cm to 1.08 cm, and the threshold of minimum updraft velocity changes from 11.5 m·s-1 to 21.2 m·s-1. The results show a general understanding on the change of 0℃ layer height to hail melting, which can provide a reference for hail forecast and hail suppression operation, and reduce the false alarm rate of WSR 88D enhanced HDA algorithm in hail size predication.
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基金项目:大连市科技局课题(2008E13SF188)资助
引用文本:
濮文耀,李红斌,宋 煜,黄 振,何 阳,赵繁盛,张殿刚,2015.0℃层高度的变化对冰雹融化影响的分析和应用[J].气象,41(8):980-985.
PU Wenyao,LI Hongbin,SONG Yu,HUANG Zhen,HE Yang,ZHAO Fansheng,ZHANG Diangang,2015.Analysis and Application of the Effect of 0℃ Layer Height on Melting Hail[J].Meteor Mon,41(8):980-985.