Improving the simulation of maize growth using WRF-Crop model based on data assimilation and local maize characteristics

IF 5.7 1区 农林科学 Q1 AGRONOMY Agricultural and Forest Meteorology Pub Date : 2025-04-15 Epub Date: 2025-03-02 DOI:10.1016/j.agrformet.2025.110478
Lun Bao , Lingxue Yu , Entao Yu , Rongping Li , Zhongquan Cai , Jiaxin Yu , Xuan Li
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Abstract

Global climate change presents a significant challenge to the sustainable development goal of eradicating hunger. Accurate assessment or projection of crop yields is crucial for ensuring food security at both global and regional levels in a changing environment. However, traditional crop models may introduce significant uncertainties due to lack of the intensified feedbacks between crop vegetation and climate systems. In this study, we coupled dynamic crop model (Noah-MP-Crop) with the Weather Research and Forecasting (WRF) model (WRF-Crop) based on data assimilation and local maize characteristics to simulate dynamic maize growth and subsequent yield at Jilin Province, China. We utilized in-site phenological observation data to refine the model's cumulative growing degree days (GDDs), and employed leaf mass assimilation to enhance the accuracy of crop phenology cycles. Our findings suggest that refining the model's GDDs thresholds and incorporating data assimilation leads to better alignment with MODIS-observed Leaf area index (LAI), evapotranspiration (ET), and gross primary productivity (GPP), with a reduction in the mean absolute error of 41.2 %, 14.1 %, and 27.5 %, respectively. The in-site eddy covariance flux observation data on soil moisture (layer 1 R = 0.9) and GPP (R = 0.82) also support our results. With the improvement of the maize growth cycles, the adjusted WRF-Crop model exhibited significantly improved accuracy in simulating maize yield, averaging 10,140 kg/ha in Jilin Province. This represents an approximate 9.26 % increase in accuracy compared to the default model configuration. Therefore, the dynamic crop-coupled WRF-Crop model showcases substantial potential for regional crop yield estimation and predictions, featuring dynamic downscaling capabilities through the incorporation of interactions between crops and the atmosphere.
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基于数据同化和本地玉米特性的WRF-Crop模型对玉米生长模拟的改进
全球气候变化对消除饥饿的可持续发展目标提出了重大挑战。在不断变化的环境中,准确评估或预测作物产量对于确保全球和区域层面的粮食安全至关重要。然而,传统的作物模式由于缺乏作物植被与气候系统之间的强烈反馈,可能会带来很大的不确定性。本研究基于数据同化和当地玉米特征,将动态作物模型(Noah-MP-Crop)与气象研究与预报(WRF- crop)模型(WRF- crop)耦合,模拟了中国吉林省玉米的动态生长和后续产量。利用现场物候观测数据对模型的累积生长度日数进行细化,并利用叶片质量同化技术提高作物物候周期的准确性。我们的研究结果表明,改进模型的gds阈值并纳入数据同化可以更好地与modis观测的叶面积指数(LAI)、蒸散发(ET)和总初级生产力(GPP)保持一致,平均绝对误差分别降低41.2%、14.1%和27.5%。土壤湿度(第一层R = 0.9)和GPP (R = 0.82)的现场涡动相关通量观测数据也支持我们的研究结果。随着玉米生长周期的改善,调整后的WRF-Crop模型对玉米产量的模拟精度显著提高,在吉林省平均为10140 kg/ha。与默认模型配置相比,这表示精度提高了大约9.26%。因此,动态作物耦合WRF-Crop模式显示了区域作物产量估计和预测的巨大潜力,通过纳入作物与大气之间的相互作用,具有动态降尺度能力。
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来源期刊
CiteScore
10.30
自引率
9.70%
发文量
415
审稿时长
69 days
期刊介绍: Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published. Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.
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