A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra

A new retrieval scheme for cloud optical thickness, effective radius, and thermodynamic phase was developed for ground-based measurements of cloud shortwave solar spectral transmittance. Fifteen parameters were derived to quantify spectral variations in shortwave transmittance due to absorpt...

Full description

Bibliographic Details
Main Authors: S. E. LeBlanc, P. Pilewskie, K. S. Schmidt, O. Coddington
Format: Article
Language:English
Published: Copernicus Publications 2015-03-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/8/1361/2015/amt-8-1361-2015.pdf
_version_ 1818000327102693376
author S. E. LeBlanc
P. Pilewskie
K. S. Schmidt
O. Coddington
author_facet S. E. LeBlanc
P. Pilewskie
K. S. Schmidt
O. Coddington
author_sort S. E. LeBlanc
collection DOAJ
description A new retrieval scheme for cloud optical thickness, effective radius, and thermodynamic phase was developed for ground-based measurements of cloud shortwave solar spectral transmittance. Fifteen parameters were derived to quantify spectral variations in shortwave transmittance due to absorption and scattering of liquid water and ice clouds, manifested by shifts in spectral slopes, curvatures, maxima, and minima. To retrieve cloud optical thickness and effective particle radius, a weighted least square fit that matched the modeled parameters was applied. The measurements for this analysis were made with the ground-based Solar Spectral Flux Radiometer in Boulder, Colorado, between May 2012 and January 2013. We compared the cloud optical thickness and effective radius from the new retrieval to two other retrieval methods. By using multiple spectral features, we find a closer fit (with a root mean square difference over the entire spectra of 3.1% for a liquid water cloud and 5.9% for an ice cloud) between measured and modeled spectra compared to two other retrieval methods which diverge by a root mean square of up to 6.4% for a liquid water cloud and 22.5% for an ice cloud. The new retrieval introduced here has an average uncertainty in effective radius (± 1.2 μm) smaller by factor of at least 2.5 than two other methods when applied to an ice cloud.
first_indexed 2024-04-14T03:20:24Z
format Article
id doaj.art-edd5ba5c94e24ecea7250a67c5b1e49b
institution Directory Open Access Journal
issn 1867-1381
1867-8548
language English
last_indexed 2024-04-14T03:20:24Z
publishDate 2015-03-01
publisher Copernicus Publications
record_format Article
series Atmospheric Measurement Techniques
spelling doaj.art-edd5ba5c94e24ecea7250a67c5b1e49b2022-12-22T02:15:19ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482015-03-01831361138310.5194/amt-8-1361-2015A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectraS. E. LeBlanc0P. Pilewskie1K. S. Schmidt2O. Coddington3University of Colorado, Department of Atmospheric and Oceanic Sciences, Boulder, CO, USAUniversity of Colorado, Department of Atmospheric and Oceanic Sciences, Boulder, CO, USAUniversity of Colorado, Laboratory for Atmospheric and Space Physics, Boulder, CO, USAUniversity of Colorado, Laboratory for Atmospheric and Space Physics, Boulder, CO, USAA new retrieval scheme for cloud optical thickness, effective radius, and thermodynamic phase was developed for ground-based measurements of cloud shortwave solar spectral transmittance. Fifteen parameters were derived to quantify spectral variations in shortwave transmittance due to absorption and scattering of liquid water and ice clouds, manifested by shifts in spectral slopes, curvatures, maxima, and minima. To retrieve cloud optical thickness and effective particle radius, a weighted least square fit that matched the modeled parameters was applied. The measurements for this analysis were made with the ground-based Solar Spectral Flux Radiometer in Boulder, Colorado, between May 2012 and January 2013. We compared the cloud optical thickness and effective radius from the new retrieval to two other retrieval methods. By using multiple spectral features, we find a closer fit (with a root mean square difference over the entire spectra of 3.1% for a liquid water cloud and 5.9% for an ice cloud) between measured and modeled spectra compared to two other retrieval methods which diverge by a root mean square of up to 6.4% for a liquid water cloud and 22.5% for an ice cloud. The new retrieval introduced here has an average uncertainty in effective radius (± 1.2 μm) smaller by factor of at least 2.5 than two other methods when applied to an ice cloud.http://www.atmos-meas-tech.net/8/1361/2015/amt-8-1361-2015.pdf
spellingShingle S. E. LeBlanc
P. Pilewskie
K. S. Schmidt
O. Coddington
A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra
Atmospheric Measurement Techniques
title A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra
title_full A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra
title_fullStr A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra
title_full_unstemmed A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra
title_short A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra
title_sort spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra
url http://www.atmos-meas-tech.net/8/1361/2015/amt-8-1361-2015.pdf
work_keys_str_mv AT seleblanc aspectralmethodfordiscriminatingthermodynamicphaseandretrievingcloudopticalthicknessandeffectiveradiususingtransmittedsolarradiancespectra
AT ppilewskie aspectralmethodfordiscriminatingthermodynamicphaseandretrievingcloudopticalthicknessandeffectiveradiususingtransmittedsolarradiancespectra
AT ksschmidt aspectralmethodfordiscriminatingthermodynamicphaseandretrievingcloudopticalthicknessandeffectiveradiususingtransmittedsolarradiancespectra
AT ocoddington aspectralmethodfordiscriminatingthermodynamicphaseandretrievingcloudopticalthicknessandeffectiveradiususingtransmittedsolarradiancespectra
AT seleblanc spectralmethodfordiscriminatingthermodynamicphaseandretrievingcloudopticalthicknessandeffectiveradiususingtransmittedsolarradiancespectra
AT ppilewskie spectralmethodfordiscriminatingthermodynamicphaseandretrievingcloudopticalthicknessandeffectiveradiususingtransmittedsolarradiancespectra
AT ksschmidt spectralmethodfordiscriminatingthermodynamicphaseandretrievingcloudopticalthicknessandeffectiveradiususingtransmittedsolarradiancespectra
AT ocoddington spectralmethodfordiscriminatingthermodynamicphaseandretrievingcloudopticalthicknessandeffectiveradiususingtransmittedsolarradiancespectra