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The SMAP Level 4 Carbon Product for Monitoring Ecosystem Land–Atmosphere CO2 Exchange

机译:用于监测生态系统陆地-大气CO 2 交换的SMAP 4级碳产品

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The National Aeronautics and Space Administration's Soil Moisture Active Passive (SMAP) mission Level 4 Carbon (L4C) product provides model estimates of the Net Ecosystem CO2 exchange (NEE) incorporating SMAP soil moisture information. The L4C product includes NEE, computed as total ecosystem respiration less gross photosynthesis, at a daily time step posted to a 9-km global grid by plant functional type. Component carbon fluxes, surface soil organic carbon stocks, underlying environmental constraints, and detailed uncertainty metrics are also included. The L4C model is driven by the SMAP Level 4 Soil Moisture data assimilation product, with additional inputs from the Goddard Earth Observing System, Version 5 weather analysis, and Moderate Resolution Imaging Spectroradiometer satellite vegetation data. The L4C data record extends from March 31, 2015 to present with ongoing production and 8-12 day latency. Comparisons against concurrent global CO2 eddy flux tower measurements, satellite solar-induced canopy florescence, and other independent observation benchmarks show favorable L4C performance and accuracy, capturing the dynamic biosphere response to recent weather anomalies. Model experiments and L4C spatiotemporal variability were analyzed to understand the independent value of soil moisture and SMAP observations relative to other sources of input information. This analysis highlights the potential for microwave observations to inform models where soil moisture strongly controls land CO2 flux variability; however, skill improvement relative to flux towers is not yet discernable within the relatively short validation period. These results indicate that SMAP provides a unique and promising capability for monitoring the linked global terrestrial water and carbon cycles.
机译:国家航空航天局的土壤被动水分主动(SMAP)任务级别4碳(L4C)产品提供了结合SMAP土壤水分信息的净生态系统CO 2 交换(NEE)的模型估计。 L4C产品包括NEE(按生态系统总呼吸量减去总光合作用计算),该值在每天的时间步长上按植物功能类型发布到9公里的全球网格中。还包括组分碳通量,地表土壤有机碳储量,潜在的环境限制以及详细的不确定性指标。 L4C模型由SMAP 4级土壤水分数据同化产品驱动,另外还有来自Goddard地球观测系统,第5版天气分析和中等分辨率成像光谱仪卫星植被数据的输入。 L4C数据记录的有效期从2015年3月31日开始,一直持续到生产和8-12天的延迟。与同时进行的全球CO 2 涡流塔测量,卫星太阳诱发的冠层日光测量和其他独立观测基准的比较显示出良好的L4C性能和准确性,捕获了动态生物圈对近期天气异常的响应。分析了模型实验和L4C时空变异性,以了解相对于其他输入信息源的土壤湿度和SMAP观测值的独立性。该分析突出显示了微波观测的潜力,可为模型在土壤湿度强烈控制土地CO 2 通量变化的模型中提供参考。然而,在相对较短的验证期内,相对于通量塔的技能提升尚不明显。这些结果表明,SMAP为监测相关的全球陆地水和碳循环提供了独特而有前途的能力。

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