Abstract

Land-surface reflectance, estimated from satellite observations through atmospheric corrections, is an essential parameter for further retrieval of various high level land-surface parameters, such as leaf area index (LAI), fraction of absorbed photosynthetically active radiation (FAPAR), and surface albedo. Although great efforts have been made, land-surface reflectance products still contain considerable noise caused by, e.g., cloud or mixed-cloud pixels, which results in temporal and spatial inconsistencies in subsequent downstream products. In this study, a new method is developed to remove the residual clouds in the Moderate Resolution Imaging Spectroradiometer (MODIS) land-surface reflectance product and reconstruct time series of surface reflectance for the red, near infrared (NIR), and shortwave infrared (SWIR) bands. A smoothing method is introduced to calculate upper envelopes of vegetation indices (VIs) from the surface reflectance data and the cloud contaminated reflectance data are identified using the time series VIs and the upper envelopes of the time series VIs. Surface reflectance was then reconstructed according to cloud-free surface reflectance by incorporating the upper envelopes of the time series VIs as constraint conditions. The method was applied to reconstruct time series of surface reflectance from MODIS/TERRA surface reflectance product (MOD09A1). Temporal consistency analysis indicates that the new method can reconstruct temporally-continuous time series of land-surface reflectance. Comparisons with cloud-free MODIS/AQUA surface reflectance product (MYD09A1) over the BELMANIP (Benchmark Land Multisite Analysis and Intercomparison of Products) sites in 2003 demonstrate that the new method provides better performance for the red band (R2 = 0.8606 and RMSE = 0.0366) and NIR band (R2 = 0.6934 and RMSE = 0.0519), than the time series cloud detection (TSCD) algorithm (R2 = 0.5811 and RMSE = 0.0649; and R2 = 0.5005 and RMSE = 0.0675, respectively).

Highlights

  • Land-surface reflectance is an essential parameter to describe properties on the Earth’s surface

  • Multiple global land-surface reflectance products have been generated from data acquired by the Moderate-Resolution Imaging Spectroradiometer (MODIS) [2], Multiangle Imaging SpectroRadiometer (MISR) and VEGETATION

  • In this study a new method is developed to remove residual clouds in the MODIS land-surface reflectance product and reconstruct time series of surface reflectance in the red, near infrared (NIR) and shortwave infrared (SWIR) bands based on temporally continuous vegetation indices (VIs)

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Summary

Introduction

Land-surface reflectance is an essential parameter to describe properties on the Earth’s surface. Compared with cloud cover assessments obtained from MODIS cloud mask, the TSCD algorithm performs very well, when the land surface is stable or changing only slowly [12] These existing surface reflectance data reprocessing methods are dependent on surface reflectance in the blue band and other auxiliary information. In this study a new method is developed to remove residual clouds in the MODIS land-surface reflectance product and reconstruct time series of surface reflectance in the red, NIR and SWIR bands based on temporally continuous VIs. Vegetation index, usually obtained by mathematical combinations of satellite observations from different spectral bands, is the most commonly used and effective parameter for characterizing vegetation cover and growth status [15].

Methodology and Data
Gap filling and Smoothing of Vegetation Indices
Cloud Detection of Surface Reflectance
Surface Reflectance Reconstruction
Comparison in Space
Temporal Analysis
Discussions
Conclusions
Full Text
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