Calculation of melt pond albedos on Arctic sea ice

An analytical approximation of spectral albedo is derived for a melt pond with a Lambertian bottom assuming that Rayleigh scattering in the water is small compared to absorption. A Monte Carlo method is used to verify that scattering can he ignored in the water. This enables us to calculate pond alb...

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Published in:Polar Research
Main Authors: Makshtas, Alexander P., Podgorny, Igor A.
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 1996
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/1918
https://doi.org/10.3402/polar.v15i1.6635
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spelling ftjpolarres:oai:journals.openacademia.net:article/1918 2024-09-15T17:35:48+00:00 Calculation of melt pond albedos on Arctic sea ice Makshtas, Alexander P. Podgorny, Igor A. 1996-01-06 application/pdf https://polarresearch.net/index.php/polar/article/view/1918 https://doi.org/10.3402/polar.v15i1.6635 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/1918/5167 https://polarresearch.net/index.php/polar/article/view/1918 doi:10.3402/polar.v15i1.6635 Polar Research; Vol. 15 No. 1 (1996); 43-52 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1996 ftjpolarres https://doi.org/10.3402/polar.v15i1.6635 2024-06-28T03:10:15Z An analytical approximation of spectral albedo is derived for a melt pond with a Lambertian bottom assuming that Rayleigh scattering in the water is small compared to absorption. A Monte Carlo method is used to verify that scattering can he ignored in the water. This enables us to calculate pond albedos in the 400–700 nm wavelength hand using the analytical approximation. Model calculations and observations indicate that a step-decrease in albedo is likely t o occur when a melt pond initially forms, and melt pond albedos in the visible depend more on the structural and optical properties of the bottom than on the depth of the pond. Article in Journal/Newspaper albedo Polar Research Sea ice Polar Research Polar Research 15 1 43 52
institution Open Polar
collection Polar Research
op_collection_id ftjpolarres
language English
description An analytical approximation of spectral albedo is derived for a melt pond with a Lambertian bottom assuming that Rayleigh scattering in the water is small compared to absorption. A Monte Carlo method is used to verify that scattering can he ignored in the water. This enables us to calculate pond albedos in the 400–700 nm wavelength hand using the analytical approximation. Model calculations and observations indicate that a step-decrease in albedo is likely t o occur when a melt pond initially forms, and melt pond albedos in the visible depend more on the structural and optical properties of the bottom than on the depth of the pond.
format Article in Journal/Newspaper
author Makshtas, Alexander P.
Podgorny, Igor A.
spellingShingle Makshtas, Alexander P.
Podgorny, Igor A.
Calculation of melt pond albedos on Arctic sea ice
author_facet Makshtas, Alexander P.
Podgorny, Igor A.
author_sort Makshtas, Alexander P.
title Calculation of melt pond albedos on Arctic sea ice
title_short Calculation of melt pond albedos on Arctic sea ice
title_full Calculation of melt pond albedos on Arctic sea ice
title_fullStr Calculation of melt pond albedos on Arctic sea ice
title_full_unstemmed Calculation of melt pond albedos on Arctic sea ice
title_sort calculation of melt pond albedos on arctic sea ice
publisher Norwegian Polar Institute
publishDate 1996
url https://polarresearch.net/index.php/polar/article/view/1918
https://doi.org/10.3402/polar.v15i1.6635
genre albedo
Polar Research
Sea ice
genre_facet albedo
Polar Research
Sea ice
op_source Polar Research; Vol. 15 No. 1 (1996); 43-52
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/1918/5167
https://polarresearch.net/index.php/polar/article/view/1918
doi:10.3402/polar.v15i1.6635
op_doi https://doi.org/10.3402/polar.v15i1.6635
container_title Polar Research
container_volume 15
container_issue 1
container_start_page 43
op_container_end_page 52
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