将基于卫星的地表土壤水分和植被状况联合同化到诺亚-MP 陆面模型中

IF 5.7 Q1 ENVIRONMENTAL SCIENCES Science of Remote Sensing Pub Date : 2024-03-26 DOI:10.1016/j.srs.2024.100129
Zdenko Heyvaert , Samuel Scherrer , Wouter Dorigo , Michel Bechtold , Gabriëlle De Lannoy
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引用次数: 0

摘要

本研究探讨了将卫星获取的地表土壤水分(SSM)和植被状况纳入 Noah-MP 陆面模式的可能性。总共进行了五次数据同化(DA)试验。其中一项实验仅同化了土壤水分主动被动任务的 SSM 检索数据,两项实验仅同化了植被状况的检索数据:哥白尼全球陆地服务的叶面积指数光学检索数据或高级微波扫描辐射计 2 的 X 波段植被光学深度微波检索数据。此外,还进行了两次联合 DA 试验,每次试验都结合了 SSM 和其中一种植被产品。DA 实验与纯模型运行进行了比较,并使用土壤水分、蒸散、净生态系统交换和总初级生产力(GPP)的独立地面参考数据对所有实验进行了评估。仅同化 SSM 可改善土壤水分状况的估算(与纯模型运行相比,SSM 异常相关性中位数提高了 0.02),而同化 LAI 则主要改善了 GPP 估算(与纯模型运行相比,RMSD 中位数减少了 0.024 gC m-2 day-1)。SSM 和植被状况的联合同化在一个单一的、物理上一致的分析产品中捕捉到了这两方面的改进。DA增量表明,这种联合设置允许一种卫星产品补偿另一种产品可能引入系统的退化。此外,SSM 和 VOD DA 联合试验的估计值集合差值最小(与纯模型运行相比,SSM 差值减少了 21%)。总之,我们的研究结果凸显了多传感器和多元数据分析的潜力,在这种方法中,来自不同来源的信息被结合起来,以同时改进对几种陆地表面状态和通量的估计。
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Joint assimilation of satellite-based surface soil moisture and vegetation conditions into the Noah-MP land surface model

This study explores the potential of integrating satellite retrievals of surface soil moisture (SSM) and vegetation conditions into the Noah-MP land surface model. In total, five data assimilation (DA) experiments were carried out. One of the experiments only assimilates SSM retrievals from the Soil Moisture Active Passive mission, two experiments only assimilate retrievals of vegetation conditions: either optical retrievals of leaf area index (LAI) from the Copernicus Global Land Service, or X-band microwave-based retrievals of vegetation optical depth (VOD) from the Advanced Microwave Scanning Radiometer 2. Additionally, two joint DA experiments are performed, each incorporating SSM and one of the vegetation products. The DA experiments are compared with a model-only run, and all experiments are evaluated using independent ground reference data of soil moisture, evapotranspiration, net ecosystem exchange and gross primary production (GPP). Assimilating only SSM improves estimates of the soil moisture profile (median SSM anomaly correlation improves with 0.02 compared to a model-only run), whereas assimilating LAI predominantly improves GPP estimates (reduction in median RMSD of 0.024 gC m−2 day−1 compared to a model-only run). The joint assimilation of SSM and vegetation conditions captures both of these improvements in a single, physically consistent analysis product. The DA increments show that this combined setup allows one satellite product to compensate for potential degradations introduced into the system by the other product. Furthermore, the joint SSM and VOD DA experiment has the smallest ensemble spread in its estimates (21% reduction in SSM spread compared to a model-only run). Overall, our results underline the potential of multi-sensor and multivariate DA, in which information from different sources is combined to improve the estimates of several land surface states and fluxes simultaneously.

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