I. Introduction
In recent decades, the volume of Earth observation data has increased rapidly. The datacenters of the China National Satellite Meteorological Center (NSMC) have archived 4.126 PBs of data, and the China center for Resources Satellite Data and Application (CCRSDA) achieved more than 16 million scenes of remote sensing (RS) images up to August 2017 as reported [1]. As a typical example, data from the moderate resolution imaging spectroradiometer (MODIS) instruments onboard the satellite TERRA and AQUA have been used to study the properties of land, atmosphere, and ocean widely since been launched in December 1999 and May 2002, respectively. Each MODIS sensor produces 70 GB of raw data per day [2], from which large amount of higher level products have been generated by national aeronautics and space administration's MODIS adaptive processing system (NASA's MODAPS). Great efforts have been made to develop quantitative remote sensing models to estimate various geophysical parameters such as normalized difference vegetation index (NDVI) and aerosol optical depth (AOD), and link these massive data to different aspects of dynamic earth [3], [4]. Time-series RS data covering large areas have been extensively used to monitor the temporal and spatial changes and patterns of Earth [5], [6]. For instance, MODIS AOD dataset are used to portray the global, regional, and seasonal distribution of the AOD [7], [8]. However, the large amount of archived RS data and the relatively poor performance of compute-intensive algorithms can reduce the data utilization and delay the response [9], [10], which raise the need for effective processing methods of RS data [11].