Abstract

Reconstructing normalized difference vegetation index (NDVI) time series datasets is essential for monitoring long-term changes in terrestrial vegetation. Here, a temporal–spatial iteration (TSI) method was developed to estimate the NDVIs of contaminated pixels, based on reliable data. The NDVIs of contaminated pixels were first computed through linear interpolation of adjacent high-quality pixels in the time series. Then, the NDVIs of remaining contaminated pixels were determined based on the NDVI of a high-quality pixel located in the same ecological zone, showing the most similar NDVI change trajectories. These two steps were repeated iteratively, using the estimated NDVIs as high-quality pixels to predict undetermined NDVIs of contaminated pixels until the NDVIs of all contaminated pixels were estimated. A case study was conducted in Inner Mongolia, China. The accuracies of estimated NDVIs using TSI were higher than the asymmetric Gaussian, Savitzky–Golay, and window-regression methods. Root mean square error (RMSE) and mean absolute percent error (MAPE) decreased by 16.7%–86.6% and 18.3%–33.0%, respectively. The TSI method performed better over a range of environmental conditions, the variation of performance by the compared methods was 1.4–5 times that of the TSI method. The TSI method will be most applicable when large numbers of contaminated pixels exist.

Highlights

  • The normalized difference vegetation index (NDVI) is an important indicator of vegetation status [1,2]

  • In sub-areas 1–6 related to forest or grassland ecological zones, both Root mean square error (RMSE) and mean absolute percent error (MAPE) based on the temporal–spatial iteration (TSI) method were clearly lower than the other three methods

  • This paper proposed a TSI method to estimate the NDVIs of contaminated pixels in the MODIS13Q1

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Summary

Introduction

The normalized difference vegetation index (NDVI) is an important indicator of vegetation status [1,2]. NDVI time series datasets have been used to identify phenological characteristics, for monitoring long-term trends, for detecting abrupt changes and in multi-temporal classification [3,4,5,6]. Pixels contaminated by atmospheric conditions, sensor viewing angles, or variations in sun-surface-sensor geometry always exist in an NDVI time series dataset [7,8,9]. It is important to determine the “accurate” NDVI values of contaminated pixels because inaccurate NDVIs can result in a misinterpretation of the dynamics of terrestrial ecosystems [10,11]. Wessels et al (2007) stated that a trend [12]. The reconstruction of accurate time series datasets is essential for the use of Moderate Resolution Imaging Spectroradiometer (MODIS) MODIS13Q1, National Oceanic and Atmospheric Administration (NOAA) Global Inventory Modeling and Mapping Studies (GIMMS), NOAA Pathfinder (PAL), or Systeme Probatoire d’Observation de la Terre (SPOT) Vegetation (VGT)

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