UV/PAR radiations and DOM properties in surface coastal waters of the Canadian shelf of the Beaufort Sea during summer 2009

Surface waters from the Beaufort Sea in the Arctic Ocean were evaluated for dissolved organic carbon (DOC), and optical characteristics including UV and PAR diffuse attenuation (Kd), and chromophoric and fluorescent dissolved organic matter (CDOM & FDOM) as part of the MALINA field campaign (30...

Full description

Bibliographic Details
Published in:Biogeosciences
Main Authors: Para, J., Charrìère, Bruno, Matsuoka, Atsushi, Miller, W., Rontani, Jean-Francois, Sempere, Richard
Other Authors: CE, Institut méditerranéen d'océanologie (MIO), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'océanographie de Villefranche (LOV), Observatoire océanologique de Villefranche-sur-mer (OOVM), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS), The publication of this article is financed by CNRS-INSU, MALINA, ANR-08-BLAN-0308,Malina,How changes in ice cover, permafrost and UV radiation impact on biodiversity and biogeochemical fluxes in the Arctic Ocean(2008)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2013
Subjects:
UV
DOC
Online Access:https://hal.science/hal-00808123
https://hal.science/hal-00808123/document
https://hal.science/hal-00808123/file/bg-10-2761-2013.pdf
https://doi.org/10.5194/bg-10-2761-2013
id ftanrparis:oai:HAL:hal-00808123v1
record_format openpolar
institution Open Polar
collection Portail HAL-ANR (Agence Nationale de la Recherche)
op_collection_id ftanrparis
language English
topic UV
PAR radiations
CDOM
DOC
Arctic ocean
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle UV
PAR radiations
CDOM
DOC
Arctic ocean
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE.MCG]Environmental Sciences/Global Changes
Para, J.
Charrìère, Bruno
Matsuoka, Atsushi
Miller, W.
Rontani, Jean-Francois
Sempere, Richard
UV/PAR radiations and DOM properties in surface coastal waters of the Canadian shelf of the Beaufort Sea during summer 2009
topic_facet UV
PAR radiations
CDOM
DOC
Arctic ocean
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE.MCG]Environmental Sciences/Global Changes
description Surface waters from the Beaufort Sea in the Arctic Ocean were evaluated for dissolved organic carbon (DOC), and optical characteristics including UV and PAR diffuse attenuation (Kd), and chromophoric and fluorescent dissolved organic matter (CDOM & FDOM) as part of the MALINA field campaign (30 July to 27 August). Spectral absorption coefficients (aCDOM(350 nm) (m-1)) were significantly correlated to both diffuse attenuation coefficients (Kd) in the UV-A and UV-B and to DOC concentrations. This indicates CDOM as the dominant attenuator of both UV-PAR solar radiation and suggests its use as an optical proxy for DOC concentrations in this region. While the Mackenzie input is the main driver of CDOM dynamics in low salinity waters, locally, primary production can create significant increases in CDOM. Extrapolating CDOM to DOC relationships, we estimate that ~16% of the DOC in the Mackenzie River does not absorb radiation at 350nm. The discharge of DOC and it chromophoric subset (CDOM) by the Mackenzie River during the MALINA cruise are estimated as ~ 0.22 TgC and 0.18 TgC, respectively. Three dissolved fluorescent components (C1-C3) were identified by fluorescence Excitation/Emission Matrix Spectroscopy (EEMS) and PARAFAC analysis. Our results showed an aquatic DOM component (C1), probably produced in numerous lakes of the watershed, that co-dominated with a terrestrial humic-like component (C2) in the Mackenzie Delta Sector. This aquatic DOM could partially explain the high CDOM spectral slopes observed in the Beaufort Sea.
author2 CE
Institut méditerranéen d'océanologie (MIO)
Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire d'océanographie de Villefranche (LOV)
Observatoire océanologique de Villefranche-sur-mer (OOVM)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)
The publication of this article is financed by CNRS-INSU
MALINA
ANR-08-BLAN-0308,Malina,How changes in ice cover, permafrost and UV radiation impact on biodiversity and biogeochemical fluxes in the Arctic Ocean(2008)
format Article in Journal/Newspaper
author Para, J.
Charrìère, Bruno
Matsuoka, Atsushi
Miller, W.
Rontani, Jean-Francois
Sempere, Richard
author_facet Para, J.
Charrìère, Bruno
Matsuoka, Atsushi
Miller, W.
Rontani, Jean-Francois
Sempere, Richard
author_sort Para, J.
title UV/PAR radiations and DOM properties in surface coastal waters of the Canadian shelf of the Beaufort Sea during summer 2009
title_short UV/PAR radiations and DOM properties in surface coastal waters of the Canadian shelf of the Beaufort Sea during summer 2009
title_full UV/PAR radiations and DOM properties in surface coastal waters of the Canadian shelf of the Beaufort Sea during summer 2009
title_fullStr UV/PAR radiations and DOM properties in surface coastal waters of the Canadian shelf of the Beaufort Sea during summer 2009
title_full_unstemmed UV/PAR radiations and DOM properties in surface coastal waters of the Canadian shelf of the Beaufort Sea during summer 2009
title_sort uv/par radiations and dom properties in surface coastal waters of the canadian shelf of the beaufort sea during summer 2009
publisher HAL CCSD
publishDate 2013
url https://hal.science/hal-00808123
https://hal.science/hal-00808123/document
https://hal.science/hal-00808123/file/bg-10-2761-2013.pdf
https://doi.org/10.5194/bg-10-2761-2013
genre Arctic Ocean
Beaufort Sea
Mackenzie Delta
Mackenzie river
genre_facet Arctic Ocean
Beaufort Sea
Mackenzie Delta
Mackenzie river
op_source ISSN: 1726-4170
EISSN: 1726-4189
Biogeosciences
https://hal.science/hal-00808123
Biogeosciences, 2013, 10, pp.2761-2774. ⟨10.5194/bg-10-2761-2013⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-10-2761-2013
hal-00808123
https://hal.science/hal-00808123
https://hal.science/hal-00808123/document
https://hal.science/hal-00808123/file/bg-10-2761-2013.pdf
doi:10.5194/bg-10-2761-2013
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/bg-10-2761-2013
container_title Biogeosciences
container_volume 10
container_issue 4
container_start_page 2761
op_container_end_page 2774
_version_ 1810429438740922368
spelling ftanrparis:oai:HAL:hal-00808123v1 2024-09-15T17:53:33+00:00 UV/PAR radiations and DOM properties in surface coastal waters of the Canadian shelf of the Beaufort Sea during summer 2009 Para, J. Charrìère, Bruno Matsuoka, Atsushi Miller, W. Rontani, Jean-Francois Sempere, Richard CE Institut méditerranéen d'océanologie (MIO) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS) Laboratoire d'océanographie de Villefranche (LOV) Observatoire océanologique de Villefranche-sur-mer (OOVM) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS) The publication of this article is financed by CNRS-INSU MALINA ANR-08-BLAN-0308,Malina,How changes in ice cover, permafrost and UV radiation impact on biodiversity and biogeochemical fluxes in the Arctic Ocean(2008) 2013 https://hal.science/hal-00808123 https://hal.science/hal-00808123/document https://hal.science/hal-00808123/file/bg-10-2761-2013.pdf https://doi.org/10.5194/bg-10-2761-2013 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-10-2761-2013 hal-00808123 https://hal.science/hal-00808123 https://hal.science/hal-00808123/document https://hal.science/hal-00808123/file/bg-10-2761-2013.pdf doi:10.5194/bg-10-2761-2013 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1726-4170 EISSN: 1726-4189 Biogeosciences https://hal.science/hal-00808123 Biogeosciences, 2013, 10, pp.2761-2774. ⟨10.5194/bg-10-2761-2013⟩ UV PAR radiations CDOM DOC Arctic ocean [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2013 ftanrparis https://doi.org/10.5194/bg-10-2761-2013 2024-07-12T11:14:03Z Surface waters from the Beaufort Sea in the Arctic Ocean were evaluated for dissolved organic carbon (DOC), and optical characteristics including UV and PAR diffuse attenuation (Kd), and chromophoric and fluorescent dissolved organic matter (CDOM & FDOM) as part of the MALINA field campaign (30 July to 27 August). Spectral absorption coefficients (aCDOM(350 nm) (m-1)) were significantly correlated to both diffuse attenuation coefficients (Kd) in the UV-A and UV-B and to DOC concentrations. This indicates CDOM as the dominant attenuator of both UV-PAR solar radiation and suggests its use as an optical proxy for DOC concentrations in this region. While the Mackenzie input is the main driver of CDOM dynamics in low salinity waters, locally, primary production can create significant increases in CDOM. Extrapolating CDOM to DOC relationships, we estimate that ~16% of the DOC in the Mackenzie River does not absorb radiation at 350nm. The discharge of DOC and it chromophoric subset (CDOM) by the Mackenzie River during the MALINA cruise are estimated as ~ 0.22 TgC and 0.18 TgC, respectively. Three dissolved fluorescent components (C1-C3) were identified by fluorescence Excitation/Emission Matrix Spectroscopy (EEMS) and PARAFAC analysis. Our results showed an aquatic DOM component (C1), probably produced in numerous lakes of the watershed, that co-dominated with a terrestrial humic-like component (C2) in the Mackenzie Delta Sector. This aquatic DOM could partially explain the high CDOM spectral slopes observed in the Beaufort Sea. Article in Journal/Newspaper Arctic Ocean Beaufort Sea Mackenzie Delta Mackenzie river Portail HAL-ANR (Agence Nationale de la Recherche) Biogeosciences 10 4 2761 2774