1999Unpublished venueRequires access

Flexible, Longwave Radiative Transfer (FLRT) in Clear and Cloudy Atmospheres

Jennifer Delamere, Knut Stamnes, E. J. Mlawer, S. A. Clough

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Abstract

This paper introduces a flexible, longwave radiative transfer tool (FLRT), which can be used to create a correlated-k, multiple-scattering model for inhomogeneous atmospheres. The spectral bandwidths can be chosen by the user within the 10 to 3000 wavenumber range. FLRT provides a mechanism from which rapid radiative transfer models (RRTMs) can be generated. Rapid radiative transfer models permit accelerated calculations of radiances, fluxes and cooling rates without comprising accuracy. Such models have a variety of atmospheric radiative transfer applications. One application includes modeling radiance measurements in spectral channels of satellite or ground-based sensors.

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What this paper is about

This paper introduces a flexible, longwave radiative transfer tool (FLRT), which can be used to create a correlated-k, multiple-scattering model for inhomogeneous atmospheres. The spectral bandwidths can be chosen by the user within the 10 to 3000 wavenumber range. FLRT provides a mechanism from which rapid radiative transfer models (RRTMs) can be generated. Rapid radiative transfer models permit accelerated calculations of radiances, fluxes and cooling rates without comprising accuracy. Such models have a variety of atmospheric radiative transfer applications. One application includes modeling radiance measurements in spectral channels of satellite or ground-based sensors.

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Available abstract

This paper introduces a flexible, longwave radiative transfer tool (FLRT), which can be used to create a correlated-k, multiple-scattering model for inhomogeneous atmospheres. The spectral bandwidths can be chosen by the user within the 10 to 3000 wavenumber range. FLRT provides a mechanism from which rapid radiative transfer models (RRTMs) can be generated. Rapid radiative transfer models permit accelerated calculations of radiances, fluxes and cooling rates without comprising accuracy. Such models have a variety of atmospheric radiative transfer applications. One application includes modeling radiance measurements in spectral channels of satellite or ground-based sensors.

Key concepts: Longwave, Radiative transfer, Radiance, Atmospheric radiative transfer codes, Remote sensing, Environmental science, Satellite, Radiative flux

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