青藏高原东部牧区大-暴雪过程雪灾灾情实时预评估方法的研究  

Study on real-time predictive assessment of snowstorm disaster in eastern pastoral area of Qinghai-Tibet Plateau

作　　者：周陆生[1] 汪青春[1] 李海红[1] 张海玲[1] 李江英[1] 

机构地区：[1]青海省气象局,青海西宁810001

出　　处：《自然灾害学报》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

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.

关 键 词：青藏高原 雪灾灾情预评估 逐步回归 持续积雪日数 暴雪 降水量 平均气温 

分 类 号：P426.634[天文地球—大气科学及气象学]