Parameterization of the downward long-wave radiation at the Earth’s surface in polar regions

Various parameterization schemes for the downward long-wave radiation at the Earth's surface which have been frequently applied in sea ice and snow cover models are tested with the aid of one year's measurements at the German stations "Koldewey" and "Neumayer" in the Ar...

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Published in:Meteorologische Zeitschrift
Main Authors: Gert König-Langlo, Ernst Augstein
Format: Article in Journal/Newspaper
Language:English
Published: Borntraeger 1994
Subjects:
Online Access:https://doi.org/10.1127/metz/3/1994/343
https://doaj.org/article/476c2ece6f604fb8bf98e622d3f27f2f
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spelling ftdoajarticles:oai:doaj.org/article:476c2ece6f604fb8bf98e622d3f27f2f 2024-09-15T17:45:24+00:00 Parameterization of the downward long-wave radiation at the Earth’s surface in polar regions Gert König-Langlo Ernst Augstein 1994-12-01T00:00:00Z https://doi.org/10.1127/metz/3/1994/343 https://doaj.org/article/476c2ece6f604fb8bf98e622d3f27f2f EN eng Borntraeger http://dx.doi.org/10.1127/metz/3/1994/343 https://doaj.org/toc/0941-2948 0941-2948 doi:10.1127/metz/3/1994/343 https://doaj.org/article/476c2ece6f604fb8bf98e622d3f27f2f Meteorologische Zeitschrift, Vol 3, Iss 6, Pp 343-347 (1994) stefan-boltzmann radiation law atmospheric emissivity ice crystals arctic antarctic stefan boltzmannsche strahlungsformel atmosphärische emissivität eiskristalle arktis antarktis koldewey neumayer Meteorology. Climatology QC851-999 article 1994 ftdoajarticles https://doi.org/10.1127/metz/3/1994/343 2024-08-05T17:50:04Z Various parameterization schemes for the downward long-wave radiation at the Earth's surface which have been frequently applied in sea ice and snow cover models are tested with the aid of one year's measurements at the German stations "Koldewey" and "Neumayer" in the Arctic and Antarctic, respectively. All of these concepts are based on the Stefan-Boltzmann radiation law with an empirically derived effective atmospheric emissivity εA. Our data confirm the distinct dependency of the latter on cloudiness. But no other influences e.g. due to falling ice crystals (diamond dust) could be detected as significant. And the low level atmospheric water vapour pressure needs not be considered explicitly in the formulae. Thus, we propose a rather simple scheme for εA which is competable to the more sophisticated ones at least for polar regions. Our parameterization reproduces the observations with root mean square (RMS) deviations of less than 16 W/m2. Article in Journal/Newspaper Antarc* Antarctic Antarktis* Arktis Arktis* Sea ice Directory of Open Access Journals: DOAJ Articles Meteorologische Zeitschrift 3 6 343 347
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic stefan-boltzmann radiation law
atmospheric emissivity
ice crystals
arctic
antarctic
stefan boltzmannsche strahlungsformel
atmosphärische emissivität
eiskristalle
arktis
antarktis
koldewey
neumayer
Meteorology. Climatology
QC851-999
spellingShingle stefan-boltzmann radiation law
atmospheric emissivity
ice crystals
arctic
antarctic
stefan boltzmannsche strahlungsformel
atmosphärische emissivität
eiskristalle
arktis
antarktis
koldewey
neumayer
Meteorology. Climatology
QC851-999
Gert König-Langlo
Ernst Augstein
Parameterization of the downward long-wave radiation at the Earth’s surface in polar regions
topic_facet stefan-boltzmann radiation law
atmospheric emissivity
ice crystals
arctic
antarctic
stefan boltzmannsche strahlungsformel
atmosphärische emissivität
eiskristalle
arktis
antarktis
koldewey
neumayer
Meteorology. Climatology
QC851-999
description Various parameterization schemes for the downward long-wave radiation at the Earth's surface which have been frequently applied in sea ice and snow cover models are tested with the aid of one year's measurements at the German stations "Koldewey" and "Neumayer" in the Arctic and Antarctic, respectively. All of these concepts are based on the Stefan-Boltzmann radiation law with an empirically derived effective atmospheric emissivity εA. Our data confirm the distinct dependency of the latter on cloudiness. But no other influences e.g. due to falling ice crystals (diamond dust) could be detected as significant. And the low level atmospheric water vapour pressure needs not be considered explicitly in the formulae. Thus, we propose a rather simple scheme for εA which is competable to the more sophisticated ones at least for polar regions. Our parameterization reproduces the observations with root mean square (RMS) deviations of less than 16 W/m2.
format Article in Journal/Newspaper
author Gert König-Langlo
Ernst Augstein
author_facet Gert König-Langlo
Ernst Augstein
author_sort Gert König-Langlo
title Parameterization of the downward long-wave radiation at the Earth’s surface in polar regions
title_short Parameterization of the downward long-wave radiation at the Earth’s surface in polar regions
title_full Parameterization of the downward long-wave radiation at the Earth’s surface in polar regions
title_fullStr Parameterization of the downward long-wave radiation at the Earth’s surface in polar regions
title_full_unstemmed Parameterization of the downward long-wave radiation at the Earth’s surface in polar regions
title_sort parameterization of the downward long-wave radiation at the earth’s surface in polar regions
publisher Borntraeger
publishDate 1994
url https://doi.org/10.1127/metz/3/1994/343
https://doaj.org/article/476c2ece6f604fb8bf98e622d3f27f2f
genre Antarc*
Antarctic
Antarktis*
Arktis
Arktis*
Sea ice
genre_facet Antarc*
Antarctic
Antarktis*
Arktis
Arktis*
Sea ice
op_source Meteorologische Zeitschrift, Vol 3, Iss 6, Pp 343-347 (1994)
op_relation http://dx.doi.org/10.1127/metz/3/1994/343
https://doaj.org/toc/0941-2948
0941-2948
doi:10.1127/metz/3/1994/343
https://doaj.org/article/476c2ece6f604fb8bf98e622d3f27f2f
op_doi https://doi.org/10.1127/metz/3/1994/343
container_title Meteorologische Zeitschrift
container_volume 3
container_issue 6
container_start_page 343
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