在Noah-MP-Crop中实施响应土壤环境的动态根系分配方案:改进农业生态系统中土壤水分、作物生长和能量通量的模拟

IF 3.5 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Huimin Meng, Chesheng Zhan, Shi Hu, Zhonghe Li, Zhonghui Lin
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引用次数: 0

摘要

陆地表面模型(LSMs)中陆地-大气相互作用的可靠模拟需要真实的根系分布模型,而传统的静态根系参数化通常无法捕捉农田生态系统中的季节性根系动态。在本研究中,我们在Noah-MP-Crop框架内开发了一个土壤环境响应动态根系分布方案(SE_root),该方案明确考虑了土壤水分(SM)、温度、通气量、容重和土壤质地。对华北平原现场观测结果的评价表明,SE_root在很大程度上优于默认静态参数化(fixed_root)和指数动态参数化(Exp_root)。站点尺度模拟在捕获SM动态、叶面积指数(LAI)和潜热通量(LHF)方面具有更高的准确性,R2值始终在0.56以上。模拟的根系生物量垂直分布与田间观测结果吻合较好,约70%的根系生物量集中在40 cm以上,且随深度的增加而下降。相对于fixed_root和Exp_root方案,SM的站点尺度平均绝对误差降低了10% ~ 12%,LAI的站点尺度平均绝对误差降低了4% ~ 10%。区域模拟进一步表明,SE_root通过捕获根系生长与局部土壤约束之间的动态反馈,更好地代表了SM和LAI的空间异质性,同时LHF也有适度的改善。总体而言,纳入这种土壤响应根系参数化可以改善SM动态、根系分配、作物生长和土地-大气交换的表征。这些发现强调了明确表示农业LSMs中根-土壤相互作用的重要性,为与气候模型耦合以获取作物-气候反馈并支持可持续管理提供了强有力的途径。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Implementing a Dynamic Root Distribution Scheme Responsive to Soil Environment Into Noah-MP-Crop: Improving Simulations of Soil Water, Crop Growth, and Energy Fluxes in Agro-Ecosystems

Reliable simulation of land–atmosphere interactions in land surface models (LSMs) requires realistic root distribution modeling, yet conventional static root parameterizations often fail to capture seasonal root dynamics in cropland ecosystems. In this study, we developed a soil–environment–responsive dynamic root distribution scheme (SE_root) within the Noah-MP-Crop framework that explicitly accounts for soil moisture (SM), temperature, aeration, bulk density, and soil texture. Evaluations against in situ observations in the North China Plain demonstrated that SE_root substantially outperformed the default static (fixed_root) and exponential dynamic (Exp_root) parameterizations. Site-scale simulations exhibited improved accuracy in capturing SM dynamics, leaf area index (LAI), and latent heat flux (LHF), yielding R2 values consistently above 0.56. The simulated vertical root biomass distribution, with approximately 70% of root biomass concentrated in the upper 40 cm and declining with depth, closely matched field observations. Relative to the fixed_root and Exp_root schemes, the site-scale mean absolute errors were reduced by 10%–12% for SM and 4%–10% for LAI. Regional simulations further revealed that by capturing the dynamic feedback between root growth and local soil constraints, SE_root better represented the spatial heterogeneity of SM and LAI, alongside modest LHF improvements. Overall, incorporating this soil-responsive root parameterization improves the representation of SM dynamics, root allocation, crop growth, and land–atmosphere exchanges. These findings underscore the importance of explicitly representing root–soil interactions in agricultural LSMs, offering a robust pathway for coupling with climate models to capture crop–climate feedbacks and support sustainable management.

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来源期刊
Journal of Geophysical Research: Biogeosciences
Journal of Geophysical Research: Biogeosciences Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
5.40%
发文量
242
期刊介绍: JGR-Biogeosciences focuses on biogeosciences of the Earth system in the past, present, and future and the extension of this research to planetary studies. The emerging field of biogeosciences spans the intellectual interface between biology and the geosciences and attempts to understand the functions of the Earth system across multiple spatial and temporal scales. Studies in biogeosciences may use multiple lines of evidence drawn from diverse fields to gain a holistic understanding of terrestrial, freshwater, and marine ecosystems and extreme environments. Specific topics within the scope of the section include process-based theoretical, experimental, and field studies of biogeochemistry, biogeophysics, atmosphere-, land-, and ocean-ecosystem interactions, biomineralization, life in extreme environments, astrobiology, microbial processes, geomicrobiology, and evolutionary geobiology
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