A synthetic data set of high-spectral-resolution infrared spectra for the Arctic atmosphere

Cloud microphysical and macrophysical properties are critical for understanding the role of clouds in climate. These properties are commonly retrieved from ground-based and satellite-based infrared remote sensing instruments. However, retrieval uncertainties are difficult to quantify without a stand...

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Published in:Earth System Science Data
Main Authors: Cox, Christopher J., Rowe, Penny M., Neshyba, Steven P., Walden, Von P.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/essd-8-199-2016
https://essd.copernicus.org/articles/8/199/2016/
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spelling ftcopernicus:oai:publications.copernicus.org:essd48506 2023-05-15T14:54:48+02:00 A synthetic data set of high-spectral-resolution infrared spectra for the Arctic atmosphere Cox, Christopher J. Rowe, Penny M. Neshyba, Steven P. Walden, Von P. 2018-09-27 application/pdf https://doi.org/10.5194/essd-8-199-2016 https://essd.copernicus.org/articles/8/199/2016/ eng eng doi:10.5194/essd-8-199-2016 https://essd.copernicus.org/articles/8/199/2016/ eISSN: 1866-3516 Text 2018 ftcopernicus https://doi.org/10.5194/essd-8-199-2016 2020-07-20T16:24:09Z Cloud microphysical and macrophysical properties are critical for understanding the role of clouds in climate. These properties are commonly retrieved from ground-based and satellite-based infrared remote sensing instruments. However, retrieval uncertainties are difficult to quantify without a standard for comparison. This is particularly true over the polar regions, where surface-based data for a cloud climatology are sparse, yet clouds represent a major source of uncertainty in weather and climate models. We describe a synthetic high-spectral-resolution infrared data set that is designed to facilitate validation and development of cloud retrieval algorithms for surface- and satellite-based remote sensing instruments. Since the data set is calculated using pre-defined cloudy atmospheres, the properties of the cloud and atmospheric state are known a priori. The atmospheric state used for the simulations is drawn from radiosonde measurements made at the North Slope of Alaska (NSA) Atmospheric Radiation Measurement (ARM) site at Barrow, Alaska (71.325° N, 156.615° W), a location that is generally representative of the western Arctic. The cloud properties for each simulation are selected from statistical distributions derived from past field measurements. Upwelling (at 60 km) and downwelling (at the surface) infrared spectra are simulated for 260 cloudy cases from 50 to 3000 cm −1 (3.3 to 200 µm) at monochromatic (line-by-line) resolution at a spacing of ∼ 0.01 cm −1 using the Line-by-line Radiative Transfer Model (LBLRTM) and the discrete-ordinate-method radiative transfer code (DISORT). These spectra are freely available for interested researchers from the NSF Arctic Data Center data repository ( doi:10.5065/D61J97TT ). Text Arctic Barrow north slope Alaska Copernicus Publications: E-Journals Arctic Earth System Science Data 8 1 199 211
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description Cloud microphysical and macrophysical properties are critical for understanding the role of clouds in climate. These properties are commonly retrieved from ground-based and satellite-based infrared remote sensing instruments. However, retrieval uncertainties are difficult to quantify without a standard for comparison. This is particularly true over the polar regions, where surface-based data for a cloud climatology are sparse, yet clouds represent a major source of uncertainty in weather and climate models. We describe a synthetic high-spectral-resolution infrared data set that is designed to facilitate validation and development of cloud retrieval algorithms for surface- and satellite-based remote sensing instruments. Since the data set is calculated using pre-defined cloudy atmospheres, the properties of the cloud and atmospheric state are known a priori. The atmospheric state used for the simulations is drawn from radiosonde measurements made at the North Slope of Alaska (NSA) Atmospheric Radiation Measurement (ARM) site at Barrow, Alaska (71.325° N, 156.615° W), a location that is generally representative of the western Arctic. The cloud properties for each simulation are selected from statistical distributions derived from past field measurements. Upwelling (at 60 km) and downwelling (at the surface) infrared spectra are simulated for 260 cloudy cases from 50 to 3000 cm −1 (3.3 to 200 µm) at monochromatic (line-by-line) resolution at a spacing of ∼ 0.01 cm −1 using the Line-by-line Radiative Transfer Model (LBLRTM) and the discrete-ordinate-method radiative transfer code (DISORT). These spectra are freely available for interested researchers from the NSF Arctic Data Center data repository ( doi:10.5065/D61J97TT ).
format Text
author Cox, Christopher J.
Rowe, Penny M.
Neshyba, Steven P.
Walden, Von P.
spellingShingle Cox, Christopher J.
Rowe, Penny M.
Neshyba, Steven P.
Walden, Von P.
A synthetic data set of high-spectral-resolution infrared spectra for the Arctic atmosphere
author_facet Cox, Christopher J.
Rowe, Penny M.
Neshyba, Steven P.
Walden, Von P.
author_sort Cox, Christopher J.
title A synthetic data set of high-spectral-resolution infrared spectra for the Arctic atmosphere
title_short A synthetic data set of high-spectral-resolution infrared spectra for the Arctic atmosphere
title_full A synthetic data set of high-spectral-resolution infrared spectra for the Arctic atmosphere
title_fullStr A synthetic data set of high-spectral-resolution infrared spectra for the Arctic atmosphere
title_full_unstemmed A synthetic data set of high-spectral-resolution infrared spectra for the Arctic atmosphere
title_sort synthetic data set of high-spectral-resolution infrared spectra for the arctic atmosphere
publishDate 2018
url https://doi.org/10.5194/essd-8-199-2016
https://essd.copernicus.org/articles/8/199/2016/
geographic Arctic
geographic_facet Arctic
genre Arctic
Barrow
north slope
Alaska
genre_facet Arctic
Barrow
north slope
Alaska
op_source eISSN: 1866-3516
op_relation doi:10.5194/essd-8-199-2016
https://essd.copernicus.org/articles/8/199/2016/
op_doi https://doi.org/10.5194/essd-8-199-2016
container_title Earth System Science Data
container_volume 8
container_issue 1
container_start_page 199
op_container_end_page 211
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