Abstract

Spectral vegetation index (VI) time series data have been used to monitor and characterize the Earth’s vegetative cover and its dynamics in regional to global scales [1] . VI time series data used in these analyses have been those derived from moderate resolution, polar-orbiting satellite sensors, such as Advanced Very High Resolution Radiometer (AVHRR), Moderate Resolution Imaging Spectroradiometer (MODIS), and VEGETATION [2] . Significant progresses have been made on our understanding of vegetation dynamics and their interaction with global climate with these VI time series data [3] .

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