Abstract

This study presents a new method that mitigates biases between the normalized difference vegetation index (NDVI) from geostationary (GEO) and low Earth orbit (LEO) satellites for Earth observation. The method geometrically and spectrally transforms GEO NDVI into LEO-compatible GEO NDVI, in which GEO’s off-nadir view is adjusted to a near-nadir view. First, a GEO-to-LEO NDVI transformation equation is derived using a linear mixture model of anisotropic vegetation and nonvegetation endmember spectra. The coefficients of the derived equation are a function of the endmember spectra of two sensors. The resultant equation is used to develop an NDVI transformation method in which endmember spectra are automatically computed from each sensor’s data independently and are combined to compute the coefficients. Importantly, this method does not require regression analysis using two-sensor NDVI data. The method is demonstrated using Himawari 8 Advanced Himawari Imager (AHI) data at off-nadir view and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) data at near-nadir view in middle latitude. The results show that the magnitudes of the averaged NDVI biases between AHI and MODIS for five test sites (0.016–0.026) were reduced after the transformation (<0.01). These findings indicate that the proposed method facilitates the combination of GEO and LEO NDVIs to provide NDVIs with smaller differences, except for cases in which the fraction of vegetation cover (FVC) depends on the view angle. Further investigations should be conducted to reduce the remaining errors in the transformation and to explore the feasibility of using the proposed method to predict near-real-time and near-nadir LEO vegetation index time series using GEO data.

Highlights

  • The normalized difference vegetation index (NDVI) has been used for monitoring terrestrial vegetation from the regional to the global scale [1], where the NDVI functions as a proxy indicator of biophysical parameters involving the leaf area index (LAI) and the fraction of absorbed photosynthetically active radiation (FAPAR) [2,3], among other parameters

  • We derived a GEO-to-low Earth orbit (LEO) NDVI transformation equation based on a linear mixture model of anisotropic vegetation and nonvegetation endmember spectra

  • We developed an NDVI transformation method in which endmember spectra from each set of sensor data are computed independently and subsequently combined to compute the coefficients of the transformation equation

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Summary

Introduction

The normalized difference vegetation index (NDVI) has been used for monitoring terrestrial vegetation from the regional to the global scale [1], where the NDVI functions as a proxy indicator of biophysical parameters involving the leaf area index (LAI) and the fraction of absorbed photosynthetically active radiation (FAPAR) [2,3], among other parameters. The global NDVI time series of the Advanced Very High Resolution Radiometer (AVHRR) onboard the National Oceanic and Atmospheric Administration (NOAA) polarorbiting, low Earth orbit (LEO) satellite series has been provided since the early 1980s [4,5]. Next-generation geostationary (GEO) satellites for Earth observation began operation in the 2010s and have provided highly calibrated data from optical sensors with improved. Himawari 8 launched in 2014 and the Advanced Baseline Imager (ABI) onboard Geostationary Operational Environmental Satellites (GEOSs) 16 and 17 launched in 2016 and 2018, respectively, can provide full-disk observation data in 10 min intervals and at 0.5–2 km spatial resolution [9,10]. An important aspect of the GEO data for land surface monitoring is its high temporal resolution, which enables observation of diurnal variations of reflectances and radiances as well as the mitigating effects of cloud contamination.

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