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Estimating soil thermal properties from sequences of land surface temperature using hybrid Genetic Algorithm-Finite Difference method

机译:混合遗传算法-有限差分法从地表温度序列估算土壤热力特性

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摘要

Most models used in land surface hydrology, vadose zone hydrology, and hydro-climatology require an accurate representation of soil thermal properties (soil thermal conductivity and volumetric heat capacity). Various empirical relations have been suggested to estimate soil thermal properties. However, they require many input parameters such as soil texture, mineralogical composition, porosity and water content, which are not always available from laboratory experiments and field measurements. In this paper, to overcome the above challenge, a hybrid numerical method, Genetic Algorithm-Finite Difference (GA-FD), is proposed to estimate soil thermal properties using land surface temperature (LST) as the only input. The genetic algorithm (GA) optimization method coupled with the finite difference (FD) modeling technique is a viable hybrid approach for estimating soil thermal properties. The finite difference method is employed to solve the heat diffusion equation and simulate LST, while a robust optimization technique (GA) is used to retrieve soil thermal properties by minimizing the difference between observed and simulated LST. Furthermore, a generalization of the hybrid model is developed for inhomogeneous soil, in which soil thermal properties are not constant throughout the soil slab. The proposed model is applied to the First International Satellite Land Surface Climatology Project (ISLSCP) Field Experiment (FIFE). The results show that the proposed hybrid numerical method is able to estimate soil thermal properties accurately, and therefore effectively eliminate the need for the unavailable soil parameters which are required by empirical methods for determining the soil thermal conductivity and volumetric heat capacity. Remarkably, the temporal variation of the retrieved soil thermal conductivity is consistent with the volumetric water content, even though no water content information is used in the model.
机译:陆面水文学,渗流带水文学和水文气候学中使用的大多数模型都要求准确表示土壤的热特性(土壤热导率和体积热容)。已经提出了各种经验关系来估计土壤的热性质。但是,它们需要许多输入参数,例如土壤质地,矿物组成,孔隙度和含水量,而这些参数并非总是可以从实验室实验和现场测量中获得。在本文中,为克服上述挑战,提出了一种混合数值方法,即遗传算法-有限差分(GA-FD),它以地表温度(LST)作为唯一输入来估算土壤的热性质。遗传算法(GA)优化方法与有限差分(FD)建模技术相结合是一种可行的混合方法,可用于估算土壤热特性。有限差分法用于求解热扩散方程并模拟LST,而鲁棒优化技术(GA)用于通过最小化观测到的LST与模拟LST之间的差异来检索土壤热特性。此外,还针对非均质土壤开发了混合模型的一般化方法,其中土壤热特性在整个土壤平板中都不恒定。提出的模型被应用于第一个国际卫星陆地表面气候学项目(ISLSCP)现场实验(FIFE)。结果表明,所提出的混合数值方法能够准确地估算土壤的热特性,从而有效地消除了经验方法确定土壤热导率和体积热容所需的土壤参数。值得注意的是,即使在模型中未使用水含量信息,所获取的土壤热导率的时间变化也与体积水含量一致。

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