Upwelling Irradiance below Sea Ice—PAR Intensities and Spectral Distributions

Upwelling and downwelling spectral (320–920 nm) distributions and photosynthetic active radiation (PAR) intensities were measured below a first-year land-fast sea ice in a western Greenland fjord with and without a snow cover. Time-series of surface upwelling PAR, downwelling PAR, and under-ice PAR...

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Published in:Journal of Marine Science and Engineering
Main Authors: Lars Chresten Lund-Hansen, Michael Bjerg-Nielsen, Tanja Stratmann, Ian Hawes, Brian K. Sorrell
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
PAR
Online Access:https://doi.org/10.3390/jmse9080830
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spelling ftmdpi:oai:mdpi.com:/2077-1312/9/8/830/ 2023-08-20T04:06:53+02:00 Upwelling Irradiance below Sea Ice—PAR Intensities and Spectral Distributions Lars Chresten Lund-Hansen Michael Bjerg-Nielsen Tanja Stratmann Ian Hawes Brian K. Sorrell agris 2021-07-30 application/pdf https://doi.org/10.3390/jmse9080830 EN eng Multidisciplinary Digital Publishing Institute Marine Environmental Science https://dx.doi.org/10.3390/jmse9080830 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 9; Issue 8; Pages: 830 sea ice upwelling and downwelling irradiances PAR low light adapted ice algae Greenland Text 2021 ftmdpi https://doi.org/10.3390/jmse9080830 2023-08-01T02:19:50Z Upwelling and downwelling spectral (320–920 nm) distributions and photosynthetic active radiation (PAR) intensities were measured below a first-year land-fast sea ice in a western Greenland fjord with and without a snow cover. Time-series of surface upwelling PAR, downwelling PAR, and under-ice PAR were also obtained. Spectral distributions of upwelling and downwelling irradiances were similar except for reduced intensities in the UV, the red, and NIR parts of the spectrum when the ice was snow-covered. Upwelling PAR amounted to about 10% of downwelling intensities, giving 5.1 µmol photons m−2 s−1 at the bottom of the ice with a snow cover and 8.2 µmol photons m−2 s−1 without. PAR partitioning analyses showed that the upwelling was related to scattering by suspended particles in the water column. A snow melt increased under-ice daily maximum downwelling PAR from 50 to 180 µmol photons m−2 s−1 and overall under-ice PAR of 55 and 198 µmol photons m−2 s−1 with 10% upwelling. It is concluded that upwelling PAR below sea ice might be an important factor regarding sea ice algae photophysiology and performance with a 10% higher PAR; specifically when PAR > Ek the light saturation point of the sea ice algae. Text Greenland ice algae Sea ice MDPI Open Access Publishing Greenland Journal of Marine Science and Engineering 9 8 830
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic sea ice
upwelling and downwelling irradiances
PAR
low light adapted ice algae
Greenland
spellingShingle sea ice
upwelling and downwelling irradiances
PAR
low light adapted ice algae
Greenland
Lars Chresten Lund-Hansen
Michael Bjerg-Nielsen
Tanja Stratmann
Ian Hawes
Brian K. Sorrell
Upwelling Irradiance below Sea Ice—PAR Intensities and Spectral Distributions
topic_facet sea ice
upwelling and downwelling irradiances
PAR
low light adapted ice algae
Greenland
description Upwelling and downwelling spectral (320–920 nm) distributions and photosynthetic active radiation (PAR) intensities were measured below a first-year land-fast sea ice in a western Greenland fjord with and without a snow cover. Time-series of surface upwelling PAR, downwelling PAR, and under-ice PAR were also obtained. Spectral distributions of upwelling and downwelling irradiances were similar except for reduced intensities in the UV, the red, and NIR parts of the spectrum when the ice was snow-covered. Upwelling PAR amounted to about 10% of downwelling intensities, giving 5.1 µmol photons m−2 s−1 at the bottom of the ice with a snow cover and 8.2 µmol photons m−2 s−1 without. PAR partitioning analyses showed that the upwelling was related to scattering by suspended particles in the water column. A snow melt increased under-ice daily maximum downwelling PAR from 50 to 180 µmol photons m−2 s−1 and overall under-ice PAR of 55 and 198 µmol photons m−2 s−1 with 10% upwelling. It is concluded that upwelling PAR below sea ice might be an important factor regarding sea ice algae photophysiology and performance with a 10% higher PAR; specifically when PAR > Ek the light saturation point of the sea ice algae.
format Text
author Lars Chresten Lund-Hansen
Michael Bjerg-Nielsen
Tanja Stratmann
Ian Hawes
Brian K. Sorrell
author_facet Lars Chresten Lund-Hansen
Michael Bjerg-Nielsen
Tanja Stratmann
Ian Hawes
Brian K. Sorrell
author_sort Lars Chresten Lund-Hansen
title Upwelling Irradiance below Sea Ice—PAR Intensities and Spectral Distributions
title_short Upwelling Irradiance below Sea Ice—PAR Intensities and Spectral Distributions
title_full Upwelling Irradiance below Sea Ice—PAR Intensities and Spectral Distributions
title_fullStr Upwelling Irradiance below Sea Ice—PAR Intensities and Spectral Distributions
title_full_unstemmed Upwelling Irradiance below Sea Ice—PAR Intensities and Spectral Distributions
title_sort upwelling irradiance below sea ice—par intensities and spectral distributions
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/jmse9080830
op_coverage agris
geographic Greenland
geographic_facet Greenland
genre Greenland
ice algae
Sea ice
genre_facet Greenland
ice algae
Sea ice
op_source Journal of Marine Science and Engineering; Volume 9; Issue 8; Pages: 830
op_relation Marine Environmental Science
https://dx.doi.org/10.3390/jmse9080830
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/jmse9080830
container_title Journal of Marine Science and Engineering
container_volume 9
container_issue 8
container_start_page 830
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