乌鲁木齐河山区流域径流形成的实验研究  

AN EXPERIMENTAL STUDY ON RUNOFF FORMATIONIN THE MOUNTAINOUS BASIN OFTHE RMQI RIVER

作　　者：康尔泗[1] 施雅风[1] 杨大庆[1] 张寅生[1] 张国威 

机构地区：[1]中国科学院兰州冰川冻土研究所 [2]新疆维吾尔自治区水文水资源局

出　　处：《第四纪研究》1997年第2期139-146,共8页Quaternary Sciences

摘　　要：乌鲁木齐河山区流域较之山前平原区有着充沛的降水，是径流形成的基础。降水量随海拔增加而增加，高山带降水以固态为主，使冰川成为山区流域重要的水储存形式。降水观测误差对流域降水量和蒸发量的估算有较大影响。冰雪消融可以依据常规气象要素的参数化热通量表达式来计算。在高山草甸蒸发量的观测、计算中，蒸渗器称重法与波恩比率法较之通量－梯度法有较高的观测精度。山区流域径流系数随流域平均海拔增加而增加，高山冰川作用区在径流形成和调节中起着重要作用。Based on the observations on precipitation,ice and snow melt,evaporation and runoff in the mountainous basin of the rmqi River,which is located at the north flank of the middle Chinese Tianshan Mountains,the runoff formation processes are discussed in this paper.A systmatic underestimation is found in the precipitation measurements by the Chinese standard gauges.The annual correction factor required is 31% for the high mountain zone,14% for the middle mountains and 26% for the front of the mountains. The solid precipitation increases with altitude in the mountains,and even is summer,solid precipitation is dominant at the high mountain zone.Both summer and annual precipitation increases with altitude,and thus the precipitation in the mountainous basins is abundant compared to that in the low land in front of the mountains.The meltwater is calculated using the parameterized heat flux expressions based on the standard meteorological elements.The measurement and calculation of the evaporation from the apline meadow indicate that the weighing lysimeter and Bowen ratio methods are more accurate than the profile flux method.The yearly variation of evaporation in the mountainous basins is small,but the monthly variation is large.The maximum monthly evaporation occurs during June and July,accounting for 37% of the annual evaporation,while the evaporation from May to September accounts for 75% or more of the annual value.The precipitation,evaporation and runoff coefficients of the mountainous basins are much larger than the mean values of those in the inland river area of China.The water storage change of the mountainous basins are mostly attributed to the glacial storage change.Along with the increase of the mean altitude of the mountainous basins,the runoff and runoff coefficient also increase.

关 键 词：河流 流域 径流 降水 蒸发 乌鲁木齐河 

分 类 号：P343.1[天文地球—水文科学] P333.1[天文地球—地球物理学]