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    基于时空数据融合的季节性积雪区高分辨率地表反照率数据生成方法

    A method for generating high-resolution data on surface albedo in seasonal snow-covered areas based on spatiotemporal data fusion

    • 摘要: 季节性积雪覆盖区的地表反照率具有变化迅速和时空异质性显著的特征,现有数据受限于传感器性能和反演方法,时空分辨率较低,难以满足季节性积雪反照率时空变化过程监测的需求。针对这一问题,该文提出了一种面向季节性积雪区的地表反照率数据生成方法,将基于HJ-1 A/B, MODIS和VIIRS数据估算的地表反照率进行时空融合,生成了高时空分辨率的地表反照率数据(时间分辨率达到1 d,空间分辨率达到30 m)。研究结果表明,该方法在积雪覆盖时段的精度更高,能够显著提升地表反照率数据的时空分辨率,可更好地反映季节性积雪冻融过程导致的地表反照率快速变化和时空异质性特征,为区域水文和水资源研究提供高质量的基础数据支撑。

       

      Abstract: The surface albedo in seasonal snow-covered areas is characterized by rapid changes and significant spatiotemporal heterogeneity. Hence, surface albedo data with a high spatiotemporal resolution are required to monitor the freeze-thaw process of snow. However, constrained by sensor performance and inversion methods, existing surface albedo data exhibit a low spatiotemporal resolution, failing to meet the demand for the effective monitoring of spatiotemporal variations in seasonal snow albedo. To address this challenge, this study developed a method for generating high-resolution surface albedo data of seasonal snow-covered areas. Specifically, spatiotemporal fusion was conducted for surface albedo data estimated based on data from the Huanjing-1 A/B (HJ-1 A/B) minisatellites for environmental protection and disaster monitoring, as well as the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Visible Infrared Imaging Radiometer Suite (VIIRS) satellites. Consequently, surface albedo data with high spatiotemporal resolutions of 1 d and 30 m were generated. The results indicate that the proposed method exhibited enhanced accuracy for snow-covered periods, significantly improving the spatiotemporal resolution of surface albedo data. This method can accurately capture the rapid changes and spatiotemporal heterogeneity of surface albedo in seasonal snow freeze-thaw processes, providing high-quality fundamental data for investigating regional hydrology and water resources.

       

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