首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Dynamic mapping of snow-free vegetation and bare soil albedos at global 1km scale from 10-year analysis of MODIS satellite products
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Dynamic mapping of snow-free vegetation and bare soil albedos at global 1km scale from 10-year analysis of MODIS satellite products

机译:从MODIS卫星产品的10年分析得出全球1公里尺度上无雪植被和裸露土壤反照率的动态图

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Land surface albedo is considered to be a fundamental quantity for accurate assessment of the surface energy budget. Whereas satellite products usually provide total surface albedo, land surface models often require a separation of snow-free surface albedos of the vegetation canopy and the underlying bare soil. In this paper, visible (0.3-0.7. μm) and near infrared (0.7-5.0. μm) vegetation and bare soil albedos are retrieved from a decade of MODIS data at global scale by using a Kalman Filter-based method. The retrieved quantities show good agreement with those derived in previous studies. The main advantage of the proposed method over other approaches is that it provides albedo components efficiently throughout the year, thus allowing the seasonal cycles to be captured. This study also exploits the relationship linking the retrieved bare soil albedo to soil moisture in order to reinforce indirectly the quality of the albedo splitting. The proposed method makes it possible to update the bare soil and vegetation albedo fields in the ECOCLIMAP land cover map, the database of physiographic parameters used by Météo-France for climate and NWP modelling. The mean relative difference between the new and the old ECOCLIMAP shortwave albedos (0.3-5.0. μm) is - 8.5% at the global scale if only albedos lower than 0.5 are considered, and 41.2% otherwise. This update of the ECOCLIMAP database will have numerous NWP and climate applications for carbon, energy, and water cycle modelling.
机译:陆地表面反照率被认为是准确评估表面能收支的基本量。卫星产品通常提供总的表面反照率,而陆地表面模型通常需要将植被冠层和下面裸露的土壤的无雪表面反照率分开。在本文中,使用基于卡尔曼滤波的方法从全球十多年的MODIS数据中获取了可见的(0.3-0.7。μm)和近红外(0.7-5.0。μm)植被和裸露的土壤反照率。检索到的数量与先前研究得出的数量吻合良好。与其他方法相比,该方法的主要优势在于,它全年可有效地提供反照率分量,因此可以捕获季节性周期。这项研究还利用了将裸露的土壤反照率与土壤水分联系起来的关系,以间接增强反照率分裂的质量。所提出的方法使得有可能更新ECOCLIMAP土地覆盖图中裸露的土壤和植被反照率场,这是法国气象局用于气候和NWP建模的生理参数数据库。如果仅考虑低于0.5的反照率,则新旧ECOCLIMAP短波反照率之间的平均相对差异(0.3-5.0.μm)在全球范围内为-8.5%,否则为41.2%。 ECOCLIMAP数据库的此更新将为碳,能源和水循环建模提供大量NWP和气候应用程序。

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