Abstract

This study developed a new atmospheric correction algorithm, GeoNEX-AC, that is independent from the traditional use of spectral band ratios but dedicated to exploiting information from the diurnal variability in the hypertemporal geostationary observations. The algorithm starts by evaluating smooth segments of the diurnal time series of the top-of-atmosphere (TOA) reflectance to identify clear-sky and snow-free observations. It then attempts to retrieve the Ross-Thick–Li-Sparse (RTLS) surface bi-directional reflectance distribution function (BRDF) parameters and the daily mean atmospheric optical depth (AOD) with an atmospheric radiative transfer model (RTM) to optimally simulate the observed diurnal variability in the clear-sky TOA reflectance. Once the initial RTLS parameters are retrieved after the algorithm’s burn-in period, they serve as the prior information to estimate the AOD levels for the following days and update the surface BRDF information with the new clear-sky observations. This process is iterated through the full time span of the observations, skipping only totally cloudy days or when surface snow is detected. We tested the algorithm over various Aerosol Robotic Network (AERONET) sites and the retrieved results well agree with the ground-based measurements. This study demonstrates that the high-frequency diurnal geostationary observations contain unique information that can help to address the atmospheric correction problem from new directions.

Highlights

  • We introduce a new algorithm, which is inspired by Multiangle Implementation of Atmospheric Correction (MAIAC) and developed from its framework, to exploit the diurnal variability in geostationary observations for atmospheric correction. (In this paper we do not distinguish the differences between “diurnal” and “daytime” but may use them interchangeably.) The algorithm, named Geostationary NASA Earth Exchange (GeoNEX)-AC, is not intended to replace MAIAC as the operational algorithm for the GeoNEX L2G products but rather be a tool for diagnostic analyses

  • The Blue-band surface reflectance is ~0.5 (Figure 12), while it is typically less than 0.1 at vegetated surfaces. This implies that the regulations of atmospheric aerosol loadings on the TOA bidirectional reflectance factor (BRF) are relatively weak as compared with variations in the surface reflectance

  • We developed a new atmospheric correction algorithm, GeoNEX-AC, that is dedicated to exploiting the high temporal resolutions of the latest geostationary satellite sensors (e.g., GOES-16/17 ABI, Himawari 8/9 AHI, and Geo-KOMPSAT 2A/AMI)

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Summary

Introduction

The new geostationary sensors continuously scan Earth’s full disk every ~10 min, generating data streams of much higher temporal resolution than the Low Earth Orbit (LEO) satellites [2,3,4,5]. Such datasets provide valuable and unique opportunities for Earth monitoring [6,7]. Geostationary NASA Earth Exchange (GeoNEX) is a collaborative effort led by NASA, NOAA, and many other research institutes to explore the potential of geostationary data streams in generating rigorous and systematic science products.

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