Sid and Reva Dewberry Department of Civil, Environmental, and Infrastructure Engineering, George Mason University, Fairfax, VA 22042, USA.
Department of Geography and Geoinformation Science, George Mason University, Fairfax, VA 22042, USA.
Sensors (Basel). 2023 Mar 7;23(6):2891. doi: 10.3390/s23062891.
Soil temperature is one of the key factors to be considered in precision agriculture to increase crop production. This study is designed to compare the effectiveness of a land surface model (Noah Multiparameterization (Noah-MP)) against a traditional crop model (Environmental Policy Integrated Climate Model (EPIC)) in estimating soil temperature. A sets of soil temperature estimates, including three different EPIC simulations (i.e., using different parameterizations) and a Noah-MP simulations, is compared to ground-based measurements from across the Central Valley in California, USA, during 2000-2019. The main conclusion is that relying only on one set of model estimates may not be optimal. Furthermore, by combining different model simulations, i.e., by taking the mean of two model simulations to reconstruct a new set of soil temperature estimates, it is possible to improve the performance of the single model in terms of different statistical metrics against the reference ground observations. Containing ratio (CR), Euclidean distance (dist), and correlation co-efficient (R) calculated for the reconstructed mean improved by 52%, 58%, and 10%, respectively, compared to both model estimates. Thus, the reconstructed mean estimates are shown to be more capable of capturing soil temperature variations under different soil characteristics and across different geographical conditions when compared to the parent model simulations.
土壤温度是精准农业中需要考虑的关键因素之一,以提高作物产量。本研究旨在比较土地表面模型(Noah 多参数化模型(Noah-MP))和传统作物模型(综合环境政策气候模型(EPIC))在估计土壤温度方面的有效性。一组土壤温度估计值,包括三种不同的 EPIC 模拟(即使用不同的参数化)和 Noah-MP 模拟,与 2000-2019 年期间美国加利福尼亚州中央谷的地面测量值进行了比较。主要结论是,仅依赖一组模型估计值可能不是最优的。此外,通过结合不同的模型模拟,即通过取两个模型模拟的平均值来重建一组新的土壤温度估计值,可以提高单个模型在不同统计指标上相对于参考地面观测值的性能。与模型估计值相比,重建平均值的包含比(CR)、欧几里得距离(dist)和相关系数(R)分别提高了 52%、58%和 10%。因此,与原始模型模拟相比,重建平均值估计值在不同土壤特性和不同地理位置下更能捕捉土壤温度变化。