Abstract

A monthly mean land and snow Bidirectional Reflectance Distribution Function (BRDF) atlas for visible and near infrared parts of the spectrum has been developed for Radiative Transfer for Television Infrared Observation Satellite (TIROS) Operational Vertical sounder (TOVS) (RTTOV). The atlas follows the methodology of the RTTOV University of Wisconsin infrared land surface emissivity (UWIREMIS) atlas, i.e., it combines satellite retrievals and a principal component analysis on a dataset of hyper-spectral surface hemispherical reflectance or albedo. The current version of the BRDF atlas is based on the Collection 5 of the Moderate Resolution Imaging (MODIS) MCD43C1 Climate Modeling Grid BRDF kernel-driven model parameters product. The MCD43C1 product combines both Terra and Aqua satellites over a 16-day period of acquisition and is provided globally at 0.05° of spatial resolution. We have improved the RTTOV land surface BRDF atlas by using the last Collection 6 of MODIS product MCD43C1. We firstly found that the MODIS C6 product improved the quality index of the BRDF model as compared with that of C5. When compared with clear-sky top of atmosphere (TOA) reflectance of Spinning Enhanced Visible and InfraRed Imagers (SEVIRI) solar channels over snow-free land surfaces, we showed that the reflectances are simulated with an absolute accuracy of 3% to 5% (i.e., 0.03–0.05 in reflectance units) when either the satellite zenith angle or the solar zenith angle is below 70°, regardless of the MODIS collection. For snow-covered surfaces, we showed that the comparison with in situ snow spectral albedo is improved with C6 with an underestimation of 0.05 in the near infrared.

Highlights

  • The radiative transfer model RTTOV (Radiative Transfer for Television Infrared ObservationSatellite (TIROS) Operational Vertical sounder (TOVS) [1,2]) is the fast radiative transfer model (RTM) developed for the assimilation of satellite top of atmosphere (TOA) radiances in manyNumerical Weather Prediction (NWP) models

  • For snow-free land surfaces, we compared Spinning Enhanced Visible and InfraRed Imagers (SEVIRI) TOA reflectances at 0.6, 0.8, It is based on the last collection collection 6 (C6) of the Moderate Resolution Imaging Spectroradiometer (MODIS) MCD43C1 product

  • Been We proposed for snow-free landbysurfaces snow-covered with two types of complemented our evaluation using theand temporal frequency ofsurfaces observations every hour during daytime to estimate the performance of the Bidirectional Reflectance Distribution Function (BRDF) model as a function of the viewing and solar zenith angles as well as the scattering angles

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Summary

Introduction

The radiative transfer model RTTOV (Radiative Transfer for Television Infrared ObservationSatellite (TIROS) Operational Vertical sounder (TOVS) [1,2]) is the fast radiative transfer model (RTM) developed for the assimilation of satellite top of atmosphere (TOA) radiances in manyNumerical Weather Prediction (NWP) models. Only TOA radiances in the infrared and the microwave parts of the spectrum are assimilated in NWP models from various polar orbiting and geostationary satellites [3,4]. In version 11 [5], we extended the capability of the RTTOV model to simulate TOA radiances or reflectances for visible to near infrared (VIS/NIR) channels such as the ones of the Moderate Resolution Imaging Spectroradiometer (MODIS) onboard Aqua and Terra, the Visible Infrared Imaging Radiometer Suite (VIIRS) onboard the Suomi-National Polar-orbiting (NPP). A very promising application of fast VIS/NIR RTM simulations is already developed for weather forecasters. Simulations of VIS/NIR channels offer new insight for cases where thermal infrared or microwave parts of the spectrum are limited, such as for low clouds, fog, or aerosols

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