摘要
1999年7月26日、27日喀尔里克山南北坡的河流 ,受高温天气和山区局地暴雨的共同作用形成了一次大洪水 ,该次洪水水位高、洪量大 ,洪水过后各河流径流量显著增加。本文从地理、气象、水情各方面对该次洪水进行分析。
A flood occured in July 26 and 27 in 1999 in the river of south and north slopes of Kerliker Mountain because of high temperature and local rainstorm.It was characterized by higher flood level and larger capacity.The runoff in rivers increased obviously after the flood.The effects of geography,meteorology and water resource on the flood are analyzed.
出处
《新疆气象》
2000年第4期11-12,共2页
Bimonthly of Xinjiang Meteorology
