摘要
根据 195 1— 1998年黄河下游代表站冬季气温资料 ,统计分析了近 3 0a平均气温和气温过程变化特点及其对凌情的影响 ,并在分析负气温演变特点及其与凌情关系的基础上 ,建立了气温凌情关系式 ,同时利用 70年代以来气温、凌情资料 ,计算分析了气温变化和其它因素对凌情的影响 .
Based no the data of air temperature of the winter in the lower reaches of Yellow River, we analyzed the characteristics of average air temperature and its changes ,and the effect of air temperature on ice jam floods, and established the relational expression between the air temperature and the ice jams flood. On the basis of analyzing the change characteristic of the negative air temperature and relationship with the ice jam floods, at the same time, using the data of air temperature and ice jam flood, the effect of air temperature variation and other factors on the ice jam flood was calculated and analyzed.
出处
《冰川冻土》
CSCD
北大核心
2001年第3期323-327,共5页
Journal of Glaciology and Geocryology
基金
国家自然科学基金重点项目 ( 5 9739170 )资助
关键词
凌情
冬季
黄河下游
封河时间
气温变化
ice jams flood
temperature in winter
the lower reaches of Yellow River