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DISTRIBUTION OF RIVER RUNOFF AND ITS CLIMATE FACTORS IN AVERAGE AND EXTREME YEARS

机译:平均和极端年份河流径流的分布及其气候因子

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Schematic maps of spatial distribution of seasonal precipitation amounts and average air temperatures were obtained for the areas studied in years with normal and extreme values of annual river runoff. Data on precipitation for January–December (I–XII) and on average air temperatures for June–September (VI–IX) during 1961–1990 collected at 93 meteorological stations located along 30.20°–44.08°N and 67.20°–82.98°E, altitude 122–4?169?m above sea level, were used in the maps’ compilation. For each point-element (i.e. a meteorological station with proper data), the ordinates of an integral empirical function of distribution of probabilities P were calculated from these data for a 30-year sample period and for each year were received average values and standard deviations of P. In characteristic years were revealed, significant differences of spatial distribution of climatic factors and runoff. It was found out also that the spatial distribution of the total volume of glaciers melting is less variable in the years with extreme water yields compared to the average years. This peculiarity is very beneficial for hydropower and agriculture sectors because it provides additional natural ability to stabilize water balance of reservoirs. Piecewise multi-factor linear equations were obtained to calculate the statistical probability of glaciers’ total melting in low and high flow years as a function of geographical coordinates and the average altitude of firn boundary.
机译:获得了多年研究的区域中季节性降雨量和平均气温的空间分布示意图,这些年份的年径流量为正常值和极值。在沿30.20°-44.08°N和67.20°-82.98°E的93个气象站收集的1961-1990年1月至12月(I-12)的降水数据和6月至9月(VI-IX)的平均气温的数据在地图编辑中使用了海拔122–4?169?m的海拔高度。对于每个点元素(即具有适当数据的气象站),从这些数据中计算出30年样本期内概率分布P的积分经验函数的纵坐标,并每年获得平均值和标准偏差揭示了在特征年份,气候因子和径流的空间分布存在显着差异。还发现,与平均年份相比,在极端水产量的年份中,冰川融化总量的空间分布变化较小。这种特性对水电和农业部门非常有益,因为它提供了稳定水库水平衡的额外自然能力。得到了分段的多因子线性方程,以计算低流量和高流量年份冰川的总融化的统计概率,该概率是地理坐标和发射边界的平均高度的函数。

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