摘要
利用青藏高原东部牧区26个县气象站30a的大-暴雪过程资料,以雪灾形成的主导因子──持续积雪 日数作为灾情评估的等级标准,应用逐步回归方法,建立了冬半年持续积雪日数对大-暴雪过程的累积降水 量、平均气温、最大积雪深度和最低气温降幅4个因子的回归方程.经F检验,所有方程的回归效果达到十分 显著或显著的水平,从而建立了大-暴雪过程雪灾灾情的灾时预评估方法.通过对1996~1999年资料的对比 试用,表明这种预评估方法具有较高的精度和业务化的潜力,可作为雪灾情报服务的一种手段.
Based on the heavy snowstorm process data of 26 county stations in eastern pastoral area of Qinghai-Tibet Plateau during last 30 years, the sustained snow-cover days which is main factor of snow-disaster formation, is made as the rank standard of disaster condition. By use of stepwise regression method, a regression equation of sustained snow-cover days is established with four factors, i. e. accumulated precipitation of heavy snowstorm, average air temperature, maxiumum snow-cover depth and minimum air temperature lapse of the process. The regression efffect of the equation reaches so signifficant level via F test that it can form a snow-disaster real-time prediction assessment method of heavy snowstorm process. By means of probation from 1996 to 1999, the results show that the real-time prediction assessment method has a high assessment accuracy and operational potential, which can be made as a measure of snow-disaster information.
出处
《自然灾害学报》
CSCD
北大核心
2001年第2期58-65,共8页
Journal of Natural Disasters
基金
国家自然科学基金资助项目(49765011)
青海自然科学基金的资助项目