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A NEW, SIMPLE, GENERAL TECHNIQUE TO PREDICT SEASONAL VARIABILITY OF RIVER DISCHARGE AND LAKE TEMPERATURE FOR LAKE ECOSYSTEM MODELS

机译:预测湖水生态系统模型河流量和湖温季节变化的一种新的,简单的通用技术

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The aim of this work is to present a new technique to predict seasonal variability in tributary water discharge, lake water retention rate and lake temperature (surface and deep water temperature and stratification) when empirical data are missing, and the basic objective is to model ecosystem rather than hydrological processes. The main features of the technique are the curves (called the norms) describing the maximum (monthly) variability and the smoothing functions (the moderators) to change the maximum variability of the norms. The smoothing functions are calculated from readily available ''map parameters'' (latitude, longitude, altitude, mean annual precipitation, catchment area and lake volume). The norms apply to all lakes of a given type. The aims of this work are to present: (1) the new technique to predict seasonal variability in tributary water discharge (Q); the basic aim is to give an account of the construction of a norm and a seasonal variability moderator; (2) a model based on the same technique to predict seasonal variabilities in surface and bottom water temperature; (3) a model for the retention rate of lake water; (4) sensitivity tests illustrating how these models work, (5) examples how to use these models within the framework of a larger lake ecosystem model; and (6) examples showing that by accounting for the seasonal variability in this way, one can improve the behaviour and predictive accuracy of dynamic lake models. The seasonal moderator technique gives dimensionless expressions that may be used in dynamic models wherever one would like to account for seasonal variability in rates and coefficients. This paper is a technical account of the method. It has, however, been outside the scope to provide thorough empirical calibrations. [References: 17]
机译:这项工作的目的是提出一种新技术,以在缺少经验数据的情况下预测支流排水量,湖泊保水率和湖泊温度(地表水和深水温度及分层)的季节变化,其基本目标是对生态系统进行建模。而不是水文过程。该技术的主要特征是描述最大(每月)可变性的曲线(称为规范)和用于更改规范最大可变性的平滑函数(主持人)。平滑函数是根据容易获得的“地图参数”(纬度,经度,海拔,年平均降水量,集水面积和湖泊流量)计算得出的。规范适用于给定类型的所有湖泊。这项工作的目的是提出:(1)预测支流排水量(Q)季节变化的新技术;基本目的是说明一个规范和一个季节性变化调节器的构建; (2)基于相同技术的模型来预测地表水和底水温度的季节性变化; (3)湖泊水滞留率模型; (4)敏感性测试,说明这些模型的工作原理;(5)举例说明如何在更大的湖泊生态系统模型的框架内使用这些模型; (6)示例表明,通过以这种方式考虑季节变化,可以改善动态湖泊模型的行为和预测准确性。季节性调节器技术提供了无量纲的表达式,可在动态模型中使用,它可以解决速率和系数的季节性变化。本文是该方法的技术说明。但是,它不能提供全面的经验校准。 [参考:17]

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