Estimating underwater light regime under spatially heterogeneous sea ice in the Arctic
Abstract: The vertical diffuse attenuation coefficient for downward plane irradiance (Kd ) is an apparent optical property commonly used in primary production models to propagate incident solar radiation in the water column. In open water, estimating Kd is relatively straightforward when a vertical...
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fttriple:oai:gotriple.eu:http://hdl.handle.net/20.500.11794/34896 2023-05-15T14:58:41+02:00 Estimating underwater light regime under spatially heterogeneous sea ice in the Arctic Massicotte, Philippe Babin, Marcel Bécu, Guislain Lambert Girard, Simon Leymarie, Edouard Arctique 2018-12-19 https://hdl.handle.net/20.500.11794/34896 https://doi.org/10.3390/app8122693 en eng http://hdl.handle.net/20.500.11794/34896 http://dx.doi.org/10.3390/app8122693 other CorpusUL geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/20.500.11794/34896 https://doi.org/10.3390/app8122693 2023-01-22T17:19:20Z Abstract: The vertical diffuse attenuation coefficient for downward plane irradiance (Kd ) is an apparent optical property commonly used in primary production models to propagate incident solar radiation in the water column. In open water, estimating Kd is relatively straightforward when a vertical profile of measurements of downward irradiance, Ed, is available. In the Arctic, the ice pack is characterized by a complex mosaic composed of sea ice with snow, ridges, melt ponds, and leads. Due to the resulting spatially heterogeneous light field in the top meters of the water column, it is difficult to measure at single-point locations meaningful Kd values that allow predicting average irradiance at any depth. The main objective of this work is to propose a new method to estimate average irradiance over large spatially heterogeneous area as it would be seen by drifting phytoplankton. Using both in situ data and 3D Monte Carlo numerical simulations of radiative transfer, we show that (1) the large-area average vertical profile of downward irradiance, Ed(z), under heterogeneous sea ice cover can be represented by a single-term exponential function and (2) the vertical attenuation coefficient for upward radiance (KLu), which is up to two times less influenced by a heterogeneous incident light field than Kd in the vicinity of a melt pond, can be used as a proxy to estimate Ed(z) in the water column. Article in Journal/Newspaper Arctic Arctique* ice pack Phytoplankton Sea ice Unknown Arctic Applied Sciences 8 12 2693 |
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English |
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geo envir |
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geo envir Massicotte, Philippe Babin, Marcel Bécu, Guislain Lambert Girard, Simon Leymarie, Edouard Estimating underwater light regime under spatially heterogeneous sea ice in the Arctic |
topic_facet |
geo envir |
description |
Abstract: The vertical diffuse attenuation coefficient for downward plane irradiance (Kd ) is an apparent optical property commonly used in primary production models to propagate incident solar radiation in the water column. In open water, estimating Kd is relatively straightforward when a vertical profile of measurements of downward irradiance, Ed, is available. In the Arctic, the ice pack is characterized by a complex mosaic composed of sea ice with snow, ridges, melt ponds, and leads. Due to the resulting spatially heterogeneous light field in the top meters of the water column, it is difficult to measure at single-point locations meaningful Kd values that allow predicting average irradiance at any depth. The main objective of this work is to propose a new method to estimate average irradiance over large spatially heterogeneous area as it would be seen by drifting phytoplankton. Using both in situ data and 3D Monte Carlo numerical simulations of radiative transfer, we show that (1) the large-area average vertical profile of downward irradiance, Ed(z), under heterogeneous sea ice cover can be represented by a single-term exponential function and (2) the vertical attenuation coefficient for upward radiance (KLu), which is up to two times less influenced by a heterogeneous incident light field than Kd in the vicinity of a melt pond, can be used as a proxy to estimate Ed(z) in the water column. |
format |
Article in Journal/Newspaper |
author |
Massicotte, Philippe Babin, Marcel Bécu, Guislain Lambert Girard, Simon Leymarie, Edouard |
author_facet |
Massicotte, Philippe Babin, Marcel Bécu, Guislain Lambert Girard, Simon Leymarie, Edouard |
author_sort |
Massicotte, Philippe |
title |
Estimating underwater light regime under spatially heterogeneous sea ice in the Arctic |
title_short |
Estimating underwater light regime under spatially heterogeneous sea ice in the Arctic |
title_full |
Estimating underwater light regime under spatially heterogeneous sea ice in the Arctic |
title_fullStr |
Estimating underwater light regime under spatially heterogeneous sea ice in the Arctic |
title_full_unstemmed |
Estimating underwater light regime under spatially heterogeneous sea ice in the Arctic |
title_sort |
estimating underwater light regime under spatially heterogeneous sea ice in the arctic |
publishDate |
2018 |
url |
https://hdl.handle.net/20.500.11794/34896 https://doi.org/10.3390/app8122693 |
op_coverage |
Arctique |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Arctique* ice pack Phytoplankton Sea ice |
genre_facet |
Arctic Arctique* ice pack Phytoplankton Sea ice |
op_source |
CorpusUL |
op_relation |
http://hdl.handle.net/20.500.11794/34896 http://dx.doi.org/10.3390/app8122693 |
op_rights |
other |
op_doi |
https://doi.org/20.500.11794/34896 https://doi.org/10.3390/app8122693 |
container_title |
Applied Sciences |
container_volume |
8 |
container_issue |
12 |
container_start_page |
2693 |
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1766330809187303424 |