Model OLD0: A Physical Parameterization for Clear-Sky Downward Longwave Radiation

Abstract Downward longwave irradiance DLF is one of the main components of the surface radiation balance (SRB), but its direct measurement is currently limited. Clouds modulate its behavior, and clear-sky DLF0 is predominant in composition of the final DLF value. It is shown that in mid-latitude and...

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Main Authors: Juan Carlos Ceballos, Diego Pereira Enoré, Jaidete Monteiro de Souza, Francisco Luiz Leitão de Mesquita
Format: Article
Language:English
Published: Sociedade Brasileira de Meteorologia 2025-01-01
Series:Revista Brasileira de Meteorologia
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Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862025000100200&lng=en&tlng=en
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author Juan Carlos Ceballos
Diego Pereira Enoré
Jaidete Monteiro de Souza
Francisco Luiz Leitão de Mesquita
author_facet Juan Carlos Ceballos
Diego Pereira Enoré
Jaidete Monteiro de Souza
Francisco Luiz Leitão de Mesquita
author_sort Juan Carlos Ceballos
collection DOAJ
description Abstract Downward longwave irradiance DLF is one of the main components of the surface radiation balance (SRB), but its direct measurement is currently limited. Clouds modulate its behavior, and clear-sky DLF0 is predominant in composition of the final DLF value. It is shown that in mid-latitude and tropical atmospheres, DLF0 can be represented as the sum of fluxes from three distinct spectral regions: R1 (λ < 7.5 µm), R2 (7.5 to 14 µm), and R3 (λ > 14 µm). R1 and R3 are closely described by blackbody radiation at screen temperature (Tscr), while R2 exhibits a mean emissivity that primarily depends on total precipitable water (w). It is presented a simple yet consistent physically-based model (hereafter denoted by OLD0), suitable for estimation of DLF0 at ground level. Validation of OLD0 with ground-based data of a worldwide set of 21 stations shows fair accuracy with bias MBE lower than 6 W.m-2 and spread (standard deviation STD) lower than 12 W.m-2 for typical values DLF0 ~ 300-400 W.m-2, compatible with surface pyrgeometer measures. The proposed algorithm outperforms existing methods, achieving a mean bias error (in module |MBE|) of approximately 2.8 W.m-2. In contrast, other widely used algorithms typically exhibit |MBEs| ranging from 8.1 to 15.9 W.m-2.
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spelling doaj-art-cb99845d5def42eb9452c1c2ab7e2a312025-02-04T07:37:05ZengSociedade Brasileira de MeteorologiaRevista Brasileira de Meteorologia1982-43512025-01-014010.1590/0102-77864010033bModel OLD0: A Physical Parameterization for Clear-Sky Downward Longwave RadiationJuan Carlos CeballosDiego Pereira Enoréhttps://orcid.org/0000-0001-7001-0560Jaidete Monteiro de SouzaFrancisco Luiz Leitão de MesquitaAbstract Downward longwave irradiance DLF is one of the main components of the surface radiation balance (SRB), but its direct measurement is currently limited. Clouds modulate its behavior, and clear-sky DLF0 is predominant in composition of the final DLF value. It is shown that in mid-latitude and tropical atmospheres, DLF0 can be represented as the sum of fluxes from three distinct spectral regions: R1 (λ < 7.5 µm), R2 (7.5 to 14 µm), and R3 (λ > 14 µm). R1 and R3 are closely described by blackbody radiation at screen temperature (Tscr), while R2 exhibits a mean emissivity that primarily depends on total precipitable water (w). It is presented a simple yet consistent physically-based model (hereafter denoted by OLD0), suitable for estimation of DLF0 at ground level. Validation of OLD0 with ground-based data of a worldwide set of 21 stations shows fair accuracy with bias MBE lower than 6 W.m-2 and spread (standard deviation STD) lower than 12 W.m-2 for typical values DLF0 ~ 300-400 W.m-2, compatible with surface pyrgeometer measures. The proposed algorithm outperforms existing methods, achieving a mean bias error (in module |MBE|) of approximately 2.8 W.m-2. In contrast, other widely used algorithms typically exhibit |MBEs| ranging from 8.1 to 15.9 W.m-2.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862025000100200&lng=en&tlng=endownward longwave radiationclear sky radiationatmospheric longwave modelmodel OLD0
spellingShingle Juan Carlos Ceballos
Diego Pereira Enoré
Jaidete Monteiro de Souza
Francisco Luiz Leitão de Mesquita
Model OLD0: A Physical Parameterization for Clear-Sky Downward Longwave Radiation
Revista Brasileira de Meteorologia
downward longwave radiation
clear sky radiation
atmospheric longwave model
model OLD0
title Model OLD0: A Physical Parameterization for Clear-Sky Downward Longwave Radiation
title_full Model OLD0: A Physical Parameterization for Clear-Sky Downward Longwave Radiation
title_fullStr Model OLD0: A Physical Parameterization for Clear-Sky Downward Longwave Radiation
title_full_unstemmed Model OLD0: A Physical Parameterization for Clear-Sky Downward Longwave Radiation
title_short Model OLD0: A Physical Parameterization for Clear-Sky Downward Longwave Radiation
title_sort model old0 a physical parameterization for clear sky downward longwave radiation
topic downward longwave radiation
clear sky radiation
atmospheric longwave model
model OLD0
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862025000100200&lng=en&tlng=en
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