Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter

Reports of severe stratospheric ozone depletion over the Arctic have heightened concern about the potential impact of rising ultraviolet-B (UV-B) radiation on north polar aquatic ecosystems. Our optical measurements and modelling results indicate that the ozone-related UV-B influence on food web pro...

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Published in:ARCTIC
Main Authors: Gibson, John A.E., Vincent, Warwick F., Nieke, Barbara, Pienitz, Reinhard
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 2000
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/63925
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author Gibson, John A.E.
Vincent, Warwick F.
Nieke, Barbara
Pienitz, Reinhard
author_facet Gibson, John A.E.
Vincent, Warwick F.
Nieke, Barbara
Pienitz, Reinhard
author_sort Gibson, John A.E.
collection Unknown
container_issue 4
container_title ARCTIC
container_volume 53
description Reports of severe stratospheric ozone depletion over the Arctic have heightened concern about the potential impact of rising ultraviolet-B (UV-B) radiation on north polar aquatic ecosystems. Our optical measurements and modelling results indicate that the ozone-related UV-B influence on food web processes in the Arctic Ocean is likely to be small relative to the effects caused by variation in the concentrations of natural UV-absorbing compounds, known as chromophoric dissolved organic matter (CDOM), that enter the Arctic basin via its large river inflows. The aim of our present study was to develop and apply a simple bio-optical index that takes into account the combined effects of attenuation by atmospheric ozone and water column CDOM, and photobiological weighting for high-latitude environments such as the Arctic Ocean. To this end, we computed values for a biologically effective UV dose rate parameter ("weighted transparency" or T*) based on underwater UV measurements in high-latitude lakes and rivers that discharge into the Arctic Ocean; measured incident UV radiation at Barrow, Alaska; and published biological weighting curves for UV-induced DNA damage and UV photoinhibition of photosynthesis. The results underscore how strongly the Arctic Ocean is influenced by riverine inputs: shifts in CDOM loading (e.g., through climate change, land-use practices, or changes in ocean circulation) can cause variations in biological UV exposure of much greater magnitude than ozone-related effects. Des rapports concernant un appauvrissement sérieux de l'ozone stratosphérique au-dessus de l'Arctique ont accru les préoccupations au sujet de l'impact potentiel d'un plus fort rayonnement ultraviolet-B (UV-B) sur les écosystèmes aquatiques du pôle Nord. Nos mesures optiques et nos résultats de modélisation indiquent que l'influence de l'UV-B relié à la couche d'ozone sur les processus du réseau trophique dans l'océan Arctique est probablement faible en comparaison avec les effets dus à la variation dans les concentrations des ...
format Article in Journal/Newspaper
genre Arctic
Arctic Basin
Arctic
Arctic Ocean
Arctique*
Barrow
Climate change
Phytoplankton
Pôle Nord
Alaska
Siberia
genre_facet Arctic
Arctic Basin
Arctic
Arctic Ocean
Arctique*
Barrow
Climate change
Phytoplankton
Pôle Nord
Alaska
Siberia
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
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op_source ARCTIC; Vol. 53 No. 4 (2000): December: 341–480; 372-382
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/63925 2025-06-15T14:14:40+00:00 Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter Gibson, John A.E. Vincent, Warwick F. Nieke, Barbara Pienitz, Reinhard 2000-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/63925 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/63925/47860 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/63925 ARCTIC; Vol. 53 No. 4 (2000): December: 341–480; 372-382 1923-1245 0004-0843 Arctic CDOM DNA global change ozone depletion phytoplankton Siberia transparency ultraviolet radiation Arctique matière organique dissoute chromophore ADN changement à l’échelle planétaire phytoplancton Sibérie transparence rayonnement ultraviolet info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 2000 ftunivcalgaryojs 2025-05-27T03:29:43Z Reports of severe stratospheric ozone depletion over the Arctic have heightened concern about the potential impact of rising ultraviolet-B (UV-B) radiation on north polar aquatic ecosystems. Our optical measurements and modelling results indicate that the ozone-related UV-B influence on food web processes in the Arctic Ocean is likely to be small relative to the effects caused by variation in the concentrations of natural UV-absorbing compounds, known as chromophoric dissolved organic matter (CDOM), that enter the Arctic basin via its large river inflows. The aim of our present study was to develop and apply a simple bio-optical index that takes into account the combined effects of attenuation by atmospheric ozone and water column CDOM, and photobiological weighting for high-latitude environments such as the Arctic Ocean. To this end, we computed values for a biologically effective UV dose rate parameter ("weighted transparency" or T*) based on underwater UV measurements in high-latitude lakes and rivers that discharge into the Arctic Ocean; measured incident UV radiation at Barrow, Alaska; and published biological weighting curves for UV-induced DNA damage and UV photoinhibition of photosynthesis. The results underscore how strongly the Arctic Ocean is influenced by riverine inputs: shifts in CDOM loading (e.g., through climate change, land-use practices, or changes in ocean circulation) can cause variations in biological UV exposure of much greater magnitude than ozone-related effects. Des rapports concernant un appauvrissement sérieux de l'ozone stratosphérique au-dessus de l'Arctique ont accru les préoccupations au sujet de l'impact potentiel d'un plus fort rayonnement ultraviolet-B (UV-B) sur les écosystèmes aquatiques du pôle Nord. Nos mesures optiques et nos résultats de modélisation indiquent que l'influence de l'UV-B relié à la couche d'ozone sur les processus du réseau trophique dans l'océan Arctique est probablement faible en comparaison avec les effets dus à la variation dans les concentrations des ... Article in Journal/Newspaper Arctic Arctic Basin Arctic Arctic Ocean Arctique* Barrow Climate change Phytoplankton Pôle Nord Alaska Siberia Unknown Arctic Arctic Ocean ARCTIC 53 4
spellingShingle Arctic
CDOM
DNA
global change
ozone depletion
phytoplankton
Siberia
transparency
ultraviolet radiation
Arctique
matière organique dissoute chromophore
ADN
changement à l’échelle planétaire
phytoplancton
Sibérie
transparence
rayonnement ultraviolet
Gibson, John A.E.
Vincent, Warwick F.
Nieke, Barbara
Pienitz, Reinhard
Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter
title Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter
title_full Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter
title_fullStr Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter
title_full_unstemmed Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter
title_short Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter
title_sort control of biological exposure to uv radiation in the arctic ocean: comparison of the roles of ozone and riverine dissolved organic matter
topic Arctic
CDOM
DNA
global change
ozone depletion
phytoplankton
Siberia
transparency
ultraviolet radiation
Arctique
matière organique dissoute chromophore
ADN
changement à l’échelle planétaire
phytoplancton
Sibérie
transparence
rayonnement ultraviolet
topic_facet Arctic
CDOM
DNA
global change
ozone depletion
phytoplankton
Siberia
transparency
ultraviolet radiation
Arctique
matière organique dissoute chromophore
ADN
changement à l’échelle planétaire
phytoplancton
Sibérie
transparence
rayonnement ultraviolet
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/63925