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Study on the process of snowmelt based on the 3S technology

机译:基于3S技术的融雪过程研究

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摘要

The research on snowmelt process is very important to flood and drought calamity monitoring and forecasting, as well as to water resource management. A distributed snowmelt runoff model based on the "3S" technology has been designed and developed in this paper. The distributed snowmelt runoff model is based on energy balance and water quantity balance, which consists of three parts: grid snowmelt model, grid runoff yield model and grid catchments model. Snowmelt and runoff yield process are all based on grid scale, so the model is provided with distributing character and has strict physical mechanism. An important concept of "Unit Period of Time" was put forward in the paper for time scale conversion, and thereby developed "Degree and Cent Snowmelt Runoff Model", and gave some thoughts for the difficult problem of hydrology time scale conversion. Another important concept of "Freezing and Melting Coefficient" had also been brought forward here, which is aimed to explain the repetitive freezing and melting physical mechanism in the snowmelt period, so it has important significance to exactly hold the snowmelt process. Besides, a Snowmelt Runoff Simulating System had been developed, which adopted methods of the combination of B/S and C/S, using a great deal of remote sensing data, weather data and hydrology data, realizing the arithmetic of the model, as well as the distributed stimulation of the discharge of the typical study area, Juntanghu Basin. Validation of this model with the true measured data resulted an average relative error under 0.18, indicating that the model was able to realize simulating the process of the snowmelt well.
机译:融雪过程的研究对洪水和干旱灾害的监测和预报以及水资源管理非常重要。本文设计并开发了基于“ 3S”技术的分布式融雪径流模型。分布式融雪径流模型基于能量平衡和水量平衡,它由三个部分组成:网格融雪模型,网格径流产量模型和网格集水模型。融雪和径流产量过程均基于网格尺度,因此该模型具有分布特征,具有严格的物理机制。本文提出了一个重要的“单位时间段”概念进行时标转换,从而发展了“度和分的融雪径流模型”,并对水文时标转换的难题提出了一些思路。这里还提出了另一个重要的概念“冻结融化系数”,其目的是解释融雪期的重复融化物理机理,因此,准确掌握融雪过程具有重要意义。此外,开发了一种融雪径流模拟系统,该系统采用了B / S和C / S相结合的方法,利用了大量的遥感数据,天气数据和水文数据,还实现了模型的算法。作为Jun塘湖盆地典型研究区放电的分布式激励。用真实的测量数据对该模型进行验证,得出的平均相对误差在0.18以下,表明该模型能够实现对融雪过程的模拟。

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