Nitrous oxide in the North Atlantic Ocean

International audience In order to get a comprehensive picture of the distribution of nitrous oxide (N 2 O) in the North Atlantic Ocean, measurements of dissolved nitrous oxide were made during three cruises in the tropical, subtropical and cold-temperate North Atlantic Ocean in October/November 200...

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Main Authors: Walter, S., Bange, H. W., Breitenbach, U., Wallace, D. W. R.
Other Authors: Forschungsbereich Marine Biogeochemie, Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR)
Format: Article in Journal/Newspaper
Language:English
Published: CCSD 2006
Subjects:
Online Access:https://hal.science/hal-00297585
https://hal.science/hal-00297585v1/document
https://hal.science/hal-00297585v1/file/bg-3-607-2006.pdf
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author Walter, S.
Bange, H. W.
Breitenbach, U.
Wallace, D. W. R.
author2 Forschungsbereich Marine Biogeochemie
Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR)
author_facet Walter, S.
Bange, H. W.
Breitenbach, U.
Wallace, D. W. R.
author_sort Walter, S.
collection Institut national des sciences de l'Univers: HAL-INSU
description International audience In order to get a comprehensive picture of the distribution of nitrous oxide (N 2 O) in the North Atlantic Ocean, measurements of dissolved nitrous oxide were made during three cruises in the tropical, subtropical and cold-temperate North Atlantic Ocean in October/November 2002, March/April 2004, and May 2002, respectively. To account for the history of atmospheric N 2 O, we suggest a new depth-dependent calculation of excess N 2 O (?N 2 O). N 2 O depth profiles showed supersaturation throughout the water column with a distinct increasing trend from the cold-temperate to the tropical region. Lowest nitrous oxide concentrations, near equilibrium and with an average of 11.0±1.7 nmol L ?1 , were found in the cold-temperate North Atlantic where the profiles showed no clear maxima. Highest values up to 37.3 nmol L ?1 occurred in the tropical North Atlantic with clear maxima at approximately 400 m. A positive correlation of nitrous oxide with nitrate, as well as excess nitrous oxide with the apparent oxygen utilization (AOU), was only observed in the subtropical and tropical regions. Therefore, we conclude that the formation of nitrous oxide via nitrification occurs in the tropical region rather than in the cold-temperate region of the North Atlantic Ocean
format Article in Journal/Newspaper
genre North Atlantic
genre_facet North Atlantic
id ftinsu:oai:HAL:hal-00297585v1
institution Open Polar
language English
op_collection_id ftinsu
op_rights info:eu-repo/semantics/OpenAccess
op_source ISSN: 1726-4170
EISSN: 1726-4189
Biogeosciences
https://hal.science/hal-00297585
Biogeosciences, 2006, 3 (4), pp.607-619
publishDate 2006
publisher CCSD
record_format openpolar
spelling ftinsu:oai:HAL:hal-00297585v1 2025-05-18T14:04:37+00:00 Nitrous oxide in the North Atlantic Ocean Walter, S. Bange, H. W. Breitenbach, U. Wallace, D. W. R. Forschungsbereich Marine Biogeochemie Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR) 2006-12-01 https://hal.science/hal-00297585 https://hal.science/hal-00297585v1/document https://hal.science/hal-00297585v1/file/bg-3-607-2006.pdf en eng CCSD European Geosciences Union info:eu-repo/semantics/OpenAccess ISSN: 1726-4170 EISSN: 1726-4189 Biogeosciences https://hal.science/hal-00297585 Biogeosciences, 2006, 3 (4), pp.607-619 [PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO] [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph] [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2006 ftinsu 2025-04-21T02:19:01Z International audience In order to get a comprehensive picture of the distribution of nitrous oxide (N 2 O) in the North Atlantic Ocean, measurements of dissolved nitrous oxide were made during three cruises in the tropical, subtropical and cold-temperate North Atlantic Ocean in October/November 2002, March/April 2004, and May 2002, respectively. To account for the history of atmospheric N 2 O, we suggest a new depth-dependent calculation of excess N 2 O (?N 2 O). N 2 O depth profiles showed supersaturation throughout the water column with a distinct increasing trend from the cold-temperate to the tropical region. Lowest nitrous oxide concentrations, near equilibrium and with an average of 11.0±1.7 nmol L ?1 , were found in the cold-temperate North Atlantic where the profiles showed no clear maxima. Highest values up to 37.3 nmol L ?1 occurred in the tropical North Atlantic with clear maxima at approximately 400 m. A positive correlation of nitrous oxide with nitrate, as well as excess nitrous oxide with the apparent oxygen utilization (AOU), was only observed in the subtropical and tropical regions. Therefore, we conclude that the formation of nitrous oxide via nitrification occurs in the tropical region rather than in the cold-temperate region of the North Atlantic Ocean Article in Journal/Newspaper North Atlantic Institut national des sciences de l'Univers: HAL-INSU
spellingShingle [PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]
[SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Walter, S.
Bange, H. W.
Breitenbach, U.
Wallace, D. W. R.
Nitrous oxide in the North Atlantic Ocean
title Nitrous oxide in the North Atlantic Ocean
title_full Nitrous oxide in the North Atlantic Ocean
title_fullStr Nitrous oxide in the North Atlantic Ocean
title_full_unstemmed Nitrous oxide in the North Atlantic Ocean
title_short Nitrous oxide in the North Atlantic Ocean
title_sort nitrous oxide in the north atlantic ocean
topic [PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]
[SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
topic_facet [PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]
[SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
url https://hal.science/hal-00297585
https://hal.science/hal-00297585v1/document
https://hal.science/hal-00297585v1/file/bg-3-607-2006.pdf