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AERIs for ARM: Accuracy and Applications

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TLDR
In this paper, the authors presented the theoretical accuracy estimates of the AERI IR atmospheric emission measurements and demonstrated performance derived from data collected in the laboratory and in the field, respectively.
Abstract
Measurements from the atmospheric emitted radiance interferometer (AERI) are used within the Atmospheric Radiation Measurement (ARM) Program to improve our understanding of the atmospheric processes important for atmospheric radiation. One of the earliest ARM goals was the collection of high spectral resolution emission data for validation of radiative transfer model (RTM) calculations in the infrared (IR). Over the years, the list of applications of AERI data have grown to include remote sensing of atmospheric thermodynamic variables, atmospheric constituents, and surface properties. Fundamental to the success of these applications is the radiometric accuracy of the AERI IR atmospheric emission measurements. This paper presents the theoretical accuracy estimates of the AERI measurements and demonstrated performance derived from data collected in the laboratory and in the field.

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Journal ArticleDOI

Evaluation of four approximate methods for calculating infrared radiances in cloudy atmospheres

TL;DR: In this article, the results of two simple methods, absorption approximation and effective beam emissivity parameterization, as well as of two more elaborate methods, the multiple-stream absorption approximation with scattering effects and the delta-Eddington two-stream source function technique, are compared with the exact results of the discrete ordinate radiative transfer method.
Journal Article

Operational Comparison of the ARM SGP AERI and BN AERI Instruments

TL;DR: In early 2003, the U.S. Department of Energy's Remote Sensing Laboratory operated by Bechtel Nevada acquired a more advanced spectrometer, the BOMEM MR300 Fourier Transform Infrared as discussed by the authors.
References
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Journal ArticleDOI

Radiometric calibration of IR Fourier transform spectrometers: solution to a problem with the High-Resolution Interferometer Sounder.

TL;DR: A calibrated Fourier transform spectrometer, known as the High-Resolution Interferometer Sounder (HIS), has been flown on the NASA U-2 research aircraft to measure the infrared emission spectrum of the earth to meet high radiometric precision and accuracy requirements.
Journal ArticleDOI

The Marine-Atmospheric Emitted Radiance Interferometer: A High-Accuracy, Seagoing Infrared Spectroradiometer

TL;DR: The Marine-Atmospheric Emitted Radiance Interferometer (M-AERI) as discussed by the authors is a state-of-the-art, self-calibrating, seagoing Fourier-transform interferometric infrared spectroradiometer that is deployed on marine platforms to measure the emission spectra from the sea surface and marine atmosphere.
Journal ArticleDOI

Meteorological Applications of Temperature and Water Vapor Retrievals from the Ground-Based Atmospheric Emitted Radiance Interferometer (AERI)

TL;DR: The Atmospheric Emitted Radiance Interferometer (AERI) as mentioned in this paper is a ground-based instrument that measures high-resolution atmospheric emitted radiances from the atmosphere, which can detect vertical and temporal changes of temperature and water vapor in the planetary boundary layer.
Journal ArticleDOI

Downwelling spectral radiance observations at the SHEBA ice station: Water vapor continuum measurements from 17 to 26μm

TL;DR: In this article, an Atmospheric Emitted Radiance Interferometer (AERI) with extended longwave spectral coverage has been deployed at the SHEBA ice station 300 miles north of the Alaskan coast to measure downwelling radiances at wavelengths of 3 to 26 μm (380 to 3000 cm−1).
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