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首页> 外文期刊>Agricultural and Forest Meteorology >Estimation of net ecosystem carbon exchange for the conterminous United States by combining MODIS and AmeriFlux data
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Estimation of net ecosystem carbon exchange for the conterminous United States by combining MODIS and AmeriFlux data

机译:通过结合MODIS和AmeriFlux数据估算美国本土的净生态系统碳交换

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Eddy covariance flux towers provide continuous measurements of net ecosystem carbon exchange (NEE) for a wide range of climate and biome types. However, these measurements only represent the carbon fluxes at the scale of the tower footprint. To quantify the net exchange of carbon dioxide between the terrestrial biosphere and the atmosphere for regions or continents, flux tower measurements need to be extrapolated to these large areas. Here we used remotely sensed data from the Moderate Resolution Imaging Spectrometer (MODIS) instrument on board the National Aeronautics and Space Administration's (NASA) Terra satellite to scale up AmeriFlux NEE measurements to the continental scale. We first combined MODIS and AmeriFlux data for representative U.S. ecosystems to develop a predictive NEE model using a modified regression tree approach. The predictive model was trained and validated using eddy flux NEE data over the periods 2000-2004 and 2005-2006, respectively. We found that the model predicted NEE well (r = 0.73, p < 0.001). We then applied the model to the continental scale and estimated NEE for each 1 km x 1 km cell across the conterminous U.S. for each 8-day interval in 2005 using spatially explicit MODIS data. The model generally captured the expected spatial and seasonal patterns of NEE as deter-mined from measurements and the literature. Our study demonstrated that our empirical approach is effective for scaling up eddy flux NEE measurements to the continental scale and producing wall-to-wall NEE estimates across multiple biomes. Our estimates may provide an independent dataset from simulations with biogeochemical models and inverse modeling approaches for examining the spatiotemporal patterns of NEE and constraining terrestrial carbon budgets over large areas.
机译:涡流协方差流量塔可连续测量各种气候和生物群落类型的净生态系统碳交换量(NEE)。但是,这些测量值仅代表塔覆盖范围内的碳通量。为了量化区域或大洲在陆地生物圈和大气之间二氧化碳的净交换,通量塔测量需要外推到这些大区域。在这里,我们使用了美国国家航空航天局(NASA)Terra卫星上的中等分辨率成像光谱仪(MODIS)仪器的遥感数据,将AmeriFlux NEE测量值扩大到了大陆范围。我们首先结合了具有代表性的美国生态系统的MODIS和AmeriFlux数据,使用改进的回归树方法开发了预测性NEE模型。分别使用2000-2004年和2005-2006年的涡流NEE数据对预测模型进行了训练和验证。我们发现该模型很好地预测了NEE(r = 0.73,p <0.001)。然后,我们将该模型应用于大陆规模,并使用空间显式的MODIS数据,在2005年的每8天间隔内,在整个美国范围内,每个1 km x 1 km像元的NEE估计值。该模型通常捕获了根据测量和文献确定的预期NEE的空间和季节模式。我们的研究表明,我们的经验方法可以有效地将涡流NEE测量值扩大到大陆规模,并产生多个生物群落的逐壁NEE估计值。我们的估计可能会提供来自具有生物地球化学模型和逆建模方法的模拟的独立数据集,以检查NEE的时空模式并限制大面积的陆地碳收支。

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