下垫面对雷暴活动的影响

A. Dulzon, V. Gorbatenko
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引用次数: 1

摘要

雷暴活动的不均匀性是在相同天气过程的背景下形成的。即使在几十英里范围内,雷暴日数和雷暴时数的平均变化也会达到1.5-2倍。在地形较为平缓的地区,雷暴活动呈点状分布。以西伯利亚和哈萨克斯坦两个具有不同自然地理条件和气候条件的地区为研究对象,分析了大气-岩石圈系统不同因子对雷电活动空间分布不规则性的影响。为了揭示雷电活动在空间上不规律的原因,作者分析了以下因素对雷电活动的影响:一个地区的地理情况,如远离极地和海洋的特征、气象观测者调查半径内的地形特征、空气温度和水蒸气的弹性、下垫面温度和湿度特征、观测区域内地理场异常的数量。下垫面温湿度条件的不均匀性和地形的不均匀性是影响这两个地区雷电活动的最重要因素。
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Influence of underlying surface on thunderstorm activity
Inhomogeneity of thunderstorm activity is formed against the background of the same synoptically processes. Even within dozens of miles an average number of thunderstorm days and thunderstorm hours can be changed by 1.5-2 times. The authors focus on the spotty spatial distribution of thunderstorm activity in the regions with fairly smooth relief. Analysis of influence of different factors of atmosphere-lithosphere system on irregularity of a spatial distribution of thunder activity was carried out for two regions with different physical and geographical situation and climate: Siberia and Kazakhstan. For revealing the causes of an irregularity of thunder activity in space the analysis of influence of the following factors upon thunder activity was done by the authors: geographical situation of a region as characteristics of remoteness from poles and oceans, orographical peculiarities in a radius of survey of a meteoobserver, air temperature and resiliency of water steam, temperature and humidity characteristics of an underlying surface, quantities of geographical fields anomalies in a region of observation. Irregularity of temperature and humidity condition of underlying surface and orograpy are the most important factors, influencing thunder activity in both regions.
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