Soluble chromophores in marine snow, seawater, sea ice and frost flowers near Barrow, Alaska
International audience We measured light absorption in 42 marine snow, sea ice, seawater, brine, and frost flower samples collected during the OASIS field campaign between February 27 and April 15, 2009. Samples represented multiple sites between landfast ice and open pack ice in coastal areas appro...
Published in: | Journal of Geophysical Research: Atmospheres |
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Main Authors: | , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2012
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Online Access: | https://insu.hal.science/insu-03622104 https://insu.hal.science/insu-03622104/document https://insu.hal.science/insu-03622104/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Beine%20-%20Soluble%20chromophores%20in%20marine%20snow%20seawater%20sea%20ice%20and.pdf https://doi.org/10.1029/2011JD016650 |
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Institut national des sciences de l'Univers: HAL-INSU |
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language |
English |
topic |
[SDU]Sciences of the Universe [physics] |
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[SDU]Sciences of the Universe [physics] Beine, Harry Anastasio, Cort Domine, Florent Douglas, Thomas Barret, Manuel France, James King, Martin Hall, Sam Ullmann, Kirk Soluble chromophores in marine snow, seawater, sea ice and frost flowers near Barrow, Alaska |
topic_facet |
[SDU]Sciences of the Universe [physics] |
description |
International audience We measured light absorption in 42 marine snow, sea ice, seawater, brine, and frost flower samples collected during the OASIS field campaign between February 27 and April 15, 2009. Samples represented multiple sites between landfast ice and open pack ice in coastal areas approximately 5 km west of Barrow, Alaska. The chromophores that are most commonly measured in snow, H 2 O 2 , NO 3 - , and NO 2 - , on average account for less than 1% of sunlight absorption in our samples. Instead, light absorption is dominated by unidentified "residual" species, likely organic compounds. Light absorption coefficients for the frost flowers on first-year sea ice are, on average, 40 times larger than values for terrestrial snow samples at Barrow, suggesting very large rates of photochemical reactions in frost flowers. For our marine samples the calculated rates of sunlight absorption and OH production from known chromophores are (0.1-1.4) × 10 14 (photons cm -3 s -1 ) and (5-70) × 10 -12 (mol L -1 s -1 ), respectively. Our residual spectra are similar to spectra of marine chromophoric dissolved organic matter (CDOM), suggesting that CDOM is the dominant chromophore in our samples. Based on our light absorption measurements we estimate dissolved organic carbon (DOC) concentrations in Barrow seawater and frost flowers as approximately 130 and 360 μM C, respectively. We expect that CDOM is a major source of OH in our marine samples, and it is likely to have other significant photochemistry as well. |
author2 |
Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Takuvik International Research Laboratory Université Laval Québec (ULaval)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Beine, Harry Anastasio, Cort Domine, Florent Douglas, Thomas Barret, Manuel France, James King, Martin Hall, Sam Ullmann, Kirk |
author_facet |
Beine, Harry Anastasio, Cort Domine, Florent Douglas, Thomas Barret, Manuel France, James King, Martin Hall, Sam Ullmann, Kirk |
author_sort |
Beine, Harry |
title |
Soluble chromophores in marine snow, seawater, sea ice and frost flowers near Barrow, Alaska |
title_short |
Soluble chromophores in marine snow, seawater, sea ice and frost flowers near Barrow, Alaska |
title_full |
Soluble chromophores in marine snow, seawater, sea ice and frost flowers near Barrow, Alaska |
title_fullStr |
Soluble chromophores in marine snow, seawater, sea ice and frost flowers near Barrow, Alaska |
title_full_unstemmed |
Soluble chromophores in marine snow, seawater, sea ice and frost flowers near Barrow, Alaska |
title_sort |
soluble chromophores in marine snow, seawater, sea ice and frost flowers near barrow, alaska |
publisher |
HAL CCSD |
publishDate |
2012 |
url |
https://insu.hal.science/insu-03622104 https://insu.hal.science/insu-03622104/document https://insu.hal.science/insu-03622104/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Beine%20-%20Soluble%20chromophores%20in%20marine%20snow%20seawater%20sea%20ice%20and.pdf https://doi.org/10.1029/2011JD016650 |
genre |
Barrow Sea ice Alaska |
genre_facet |
Barrow Sea ice Alaska |
op_source |
ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://insu.hal.science/insu-03622104 Journal of Geophysical Research: Atmospheres, 2012, 117, 58, p. 73-95. ⟨10.1029/2011JD016650⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2011JD016650 insu-03622104 https://insu.hal.science/insu-03622104 https://insu.hal.science/insu-03622104/document https://insu.hal.science/insu-03622104/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Beine%20-%20Soluble%20chromophores%20in%20marine%20snow%20seawater%20sea%20ice%20and.pdf BIBCODE: 2012JGRD.117.0R15B doi:10.1029/2011JD016650 |
op_rights |
http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2011JD016650 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
117 |
container_issue |
D14 |
container_start_page |
n/a |
op_container_end_page |
n/a |
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1797580456997158912 |
spelling |
ftinsu:oai:HAL:insu-03622104v1 2024-04-28T08:14:22+00:00 Soluble chromophores in marine snow, seawater, sea ice and frost flowers near Barrow, Alaska Beine, Harry Anastasio, Cort Domine, Florent Douglas, Thomas Barret, Manuel France, James King, Martin Hall, Sam Ullmann, Kirk Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Takuvik International Research Laboratory Université Laval Québec (ULaval)-Centre National de la Recherche Scientifique (CNRS) 2012 https://insu.hal.science/insu-03622104 https://insu.hal.science/insu-03622104/document https://insu.hal.science/insu-03622104/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Beine%20-%20Soluble%20chromophores%20in%20marine%20snow%20seawater%20sea%20ice%20and.pdf https://doi.org/10.1029/2011JD016650 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2011JD016650 insu-03622104 https://insu.hal.science/insu-03622104 https://insu.hal.science/insu-03622104/document https://insu.hal.science/insu-03622104/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Beine%20-%20Soluble%20chromophores%20in%20marine%20snow%20seawater%20sea%20ice%20and.pdf BIBCODE: 2012JGRD.117.0R15B doi:10.1029/2011JD016650 http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://insu.hal.science/insu-03622104 Journal of Geophysical Research: Atmospheres, 2012, 117, 58, p. 73-95. ⟨10.1029/2011JD016650⟩ [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2012 ftinsu https://doi.org/10.1029/2011JD016650 2024-04-05T00:34:31Z International audience We measured light absorption in 42 marine snow, sea ice, seawater, brine, and frost flower samples collected during the OASIS field campaign between February 27 and April 15, 2009. Samples represented multiple sites between landfast ice and open pack ice in coastal areas approximately 5 km west of Barrow, Alaska. The chromophores that are most commonly measured in snow, H 2 O 2 , NO 3 - , and NO 2 - , on average account for less than 1% of sunlight absorption in our samples. Instead, light absorption is dominated by unidentified "residual" species, likely organic compounds. Light absorption coefficients for the frost flowers on first-year sea ice are, on average, 40 times larger than values for terrestrial snow samples at Barrow, suggesting very large rates of photochemical reactions in frost flowers. For our marine samples the calculated rates of sunlight absorption and OH production from known chromophores are (0.1-1.4) × 10 14 (photons cm -3 s -1 ) and (5-70) × 10 -12 (mol L -1 s -1 ), respectively. Our residual spectra are similar to spectra of marine chromophoric dissolved organic matter (CDOM), suggesting that CDOM is the dominant chromophore in our samples. Based on our light absorption measurements we estimate dissolved organic carbon (DOC) concentrations in Barrow seawater and frost flowers as approximately 130 and 360 μM C, respectively. We expect that CDOM is a major source of OH in our marine samples, and it is likely to have other significant photochemistry as well. Article in Journal/Newspaper Barrow Sea ice Alaska Institut national des sciences de l'Univers: HAL-INSU Journal of Geophysical Research: Atmospheres 117 D14 n/a n/a |