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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Downscaling real-time vegetation dynamics by fusing multi-temporal MODIS and Landsat NDVI in topographically complex terrain
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Downscaling real-time vegetation dynamics by fusing multi-temporal MODIS and Landsat NDVI in topographically complex terrain

机译:通过在地形复杂的地形中融合多时间MODIS和Landsat NDVI来缩减实时植被动态

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Canopy phenology is an important factor driving seasonal patterns of water and carbon exchange between land surface and atmosphere. Recent developments of real-time global satellite products (e.g., MODIS) provide the potential to assimilate dynamic canopy measurements with spatially distributed process-based ecohydrological models. However, global satellite products usually are provided with relatively coarse spatial resolutions, averaging out important spatial heterogeneity of both terrain and vegetation. Therefore, bias can result from lumped representation of ecological and hydrological processes especially in topographically complex terrain. Successful downscaling of canopy phenology to high spatial resolution would be indispensable for catchment-scale distributed ecohydrological modeling, aiming at understanding complex patterns of water, carbon and nutrient cycling in mountainous watersheds. Two downscaling approaches are developed in this study to overcome this issue by fusing multi-temporal MODIS and Landsat TM data in conjunction with topographic information to estimate high spatio-temporal resolution biophysical parameters over complex terrain. MODIS FPAR (fraction of absorbed photosynthetically active radiation) is used to provide medium spatial resolution phenology, while the variability of vegetation within a MODIS pixel is characterized by Landsat NDVI. The algorithms depend on the scale-invariant linear relationship between FPAR and NDVI, which is verified in this study. Downscaled vegetation dynamics are successfully validated both temporally and spatially with ground-based continuous FPAR and leaf area index measurements. Topographic correction during the downscaling process has a limited effect on downscaled FPAR products except for the period around the winter solstice in the study area.
机译:冠层物候是驱动陆地表面与大气之间水和碳交换的季节性模式的重要因素。实时全球卫星产品(例如MODIS)的最新发展提供了利用基于空间分布的基于过程的生态水文模型来吸收动态冠层测量的潜力。但是,全球卫星产品通常具有相对粗略的空间分辨率,可以将地形和植被的重要空间异质性平均化。因此,特别是在地形复杂的地形中,生态和水文过程的集中表示可能导致偏差。成功地将冠层物候尺度缩减到高空间分辨率对于流域规模的分布式生态水文建模是必不可少的,其目的是了解山区流域中水,碳和养分循环的复杂模式。本研究中开发了两种缩减规模的方法来解决此问题,方法是将多时相MODIS和Landsat TM数据与地形信息融合在一起,以估计复杂地形上的高时空分辨率生物物理参数。 MODIS FPAR(吸收的光合有效辐射的分数)用于提供中等的空间分辨率物候,而MODIS像素内植被的变异性由Landsat NDVI表征。该算法取决于FPAR和NDVI之间的尺度不变线性关系,这在本研究中得到了验证。通过基于地面的连续FPAR和叶面积指数测量,成功地在时间和空间上验证了缩减尺度的植被动态。降尺度过程中的地形校正对降尺度的FPAR产品的影响有限,除了研究区的冬至前后。

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