Technical note: Fu–Liou–Gu and Corti–Peter model performance evaluation for radiative retrievals from cirrus clouds

We compare, for the first time, the performance of a simplified atmospheric radiative transfer algorithm package, the Corti–Peter (CP) model, versus the more complex Fu–Liou–Gu (FLG) model, for resolving top-of-the-atmosphere radiative forcing characteristics from single-layer cirrus clouds obtai...

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Main Authors: S. Lolli, J. R. Campbell, J. R. Lewis, Y. Gu, E. J. Welton
Format: Article
Language:English
Published: Copernicus Publications 2017-06-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/17/7025/2017/acp-17-7025-2017.pdf
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spelling doaj-cda4e054b676495ebc1fb683100c71ac2020-11-24T22:31:16ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242017-06-01177025703410.5194/acp-17-7025-2017Technical note: Fu–Liou–Gu and Corti–Peter model performance evaluation for radiative retrievals from cirrus cloudsS. Lolli0S. Lolli1J. R. Campbell2J. R. Lewis3Y. Gu4E. J. Welton5NASA GSFC-JCET, Code 612, 20771 Greenbelt, MD, USACNR-IMAA, Istituto di Metodologie per l'Analisi Ambientale, Potenza, ItalyNaval Research Laboratory, Monterey, CA, USANASA GSFC-JCET, Code 612, 20771 Greenbelt, MD, USAUCLA, Los Angeles, CA, USANASA GSFC, Code 612, 20771 Greenbelt, MD, USAWe compare, for the first time, the performance of a simplified atmospheric radiative transfer algorithm package, the Corti–Peter (CP) model, versus the more complex Fu–Liou–Gu (FLG) model, for resolving top-of-the-atmosphere radiative forcing characteristics from single-layer cirrus clouds obtained from the NASA Micro-Pulse Lidar Network database in 2010 and 2011 at Singapore and in Greenbelt, Maryland, USA, in 2012. Specifically, CP simplifies calculation of both clear-sky longwave and shortwave radiation through regression analysis applied to radiative calculations, which contributes significantly to differences between the two. The results of the intercomparison show that differences in annual net top-of-the-atmosphere (TOA) cloud radiative forcing can reach 65 %. This is particularly true when land surface temperatures are warmer than 288 K, where the CP regression analysis becomes less accurate. CP proves useful for first-order estimates of TOA cirrus cloud forcing, but may not be suitable for quantitative accuracy, including the absolute sign of cirrus cloud daytime TOA forcing that can readily oscillate around zero globally.http://www.atmos-chem-phys.net/17/7025/2017/acp-17-7025-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Lolli
S. Lolli
J. R. Campbell
J. R. Lewis
Y. Gu
E. J. Welton
spellingShingle S. Lolli
S. Lolli
J. R. Campbell
J. R. Lewis
Y. Gu
E. J. Welton
Technical note: Fu–Liou–Gu and Corti–Peter model performance evaluation for radiative retrievals from cirrus clouds
Atmospheric Chemistry and Physics
author_facet S. Lolli
S. Lolli
J. R. Campbell
J. R. Lewis
Y. Gu
E. J. Welton
author_sort S. Lolli
title Technical note: Fu–Liou–Gu and Corti–Peter model performance evaluation for radiative retrievals from cirrus clouds
title_short Technical note: Fu–Liou–Gu and Corti–Peter model performance evaluation for radiative retrievals from cirrus clouds
title_full Technical note: Fu–Liou–Gu and Corti–Peter model performance evaluation for radiative retrievals from cirrus clouds
title_fullStr Technical note: Fu–Liou–Gu and Corti–Peter model performance evaluation for radiative retrievals from cirrus clouds
title_full_unstemmed Technical note: Fu–Liou–Gu and Corti–Peter model performance evaluation for radiative retrievals from cirrus clouds
title_sort technical note: fu–liou–gu and corti–peter model performance evaluation for radiative retrievals from cirrus clouds
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2017-06-01
description We compare, for the first time, the performance of a simplified atmospheric radiative transfer algorithm package, the Corti–Peter (CP) model, versus the more complex Fu–Liou–Gu (FLG) model, for resolving top-of-the-atmosphere radiative forcing characteristics from single-layer cirrus clouds obtained from the NASA Micro-Pulse Lidar Network database in 2010 and 2011 at Singapore and in Greenbelt, Maryland, USA, in 2012. Specifically, CP simplifies calculation of both clear-sky longwave and shortwave radiation through regression analysis applied to radiative calculations, which contributes significantly to differences between the two. The results of the intercomparison show that differences in annual net top-of-the-atmosphere (TOA) cloud radiative forcing can reach 65 %. This is particularly true when land surface temperatures are warmer than 288 K, where the CP regression analysis becomes less accurate. CP proves useful for first-order estimates of TOA cirrus cloud forcing, but may not be suitable for quantitative accuracy, including the absolute sign of cirrus cloud daytime TOA forcing that can readily oscillate around zero globally.
url http://www.atmos-chem-phys.net/17/7025/2017/acp-17-7025-2017.pdf
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