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Distribution type evaluation method of snow and ice water resources

机译:冰雪水资源分布类型评价方法

摘要

PPROBLEM TO BE SOLVED: To provide a distribution type of an evaluation method for snowice as a water resource such as predicting future variation by grasping a variation in accurate snowice water resource quantity in objective region and variation in outflow rate of the objective region, for example, by the eventual output, outflow rate for snowfall and snow melting in order to construct a system by verifying and correcting actual outflow and calculation outflow using a distribution type of an outflow model. PSOLUTION: The objective region is partitioned in a grid. From snowfall in each grid by meteorological data and each geographical conditions and the outflow of each grid including snow melting by a phenomenological model based on snowfall quantity, snow melting, soil penetration and evaporation, the outflow rate of the whole objective region is calculated from a pseudo river channel network by actual river data and geological data. By verifying and comparing the outflow and the actual outflow and correcting parameters for correcting the snowfall quantity in each grid and calculating the snowfall quantity, snow melting or outflow, accurate snowice water resources in the objective region is grasped with the distribution type of the evaluation method for the snowice water resources. PCOPYRIGHT: (C)2006,JPO&NCIPI
机译:

要解决的问题:提供一种用于雪水作为水资源评估方法的分布类型,例如通过掌握目标区域中准确的积雪水资源量的变化和目标区域流出量的变化来预测未来的变化例如,通过最终输出,降雪和融雪的流出率,以便通过验证和校正实际流出量并使用流出模型的分布类型计算流出量来构建系统。

解决方案:目标区域在网格中划分。根据气象数据和每个地理条件在每个网格中的降雪量以及每个网格的流出量,包括基于降雪量,融雪,土壤渗透和蒸发的现象学模型的融雪,可通过以下方法计算整个目标区域的流出率:伪河道网由实际河道数据和地质数据组成。通过验证和比较出水量和实际出水量以及用于校正每个网格中的降雪量的校正参数并计算降雪量,融雪或流出量,利用评估方法的分布类型来掌握目标区域中准确的积雪水资源为积雪的水资源。

版权:(C)2006,JPO&NCIPI

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