Impact of North Brazil Current rings on air-sea CO2 flux variability in winter 2020
The North Brazil Current (NBC) flows northward across the Equator, passes the mouth of the Amazon River, and forms large oceanic eddies near 8° N. We investigate the processes driving the variability of air-sea CO 2 fluxes at different scales in early 2020 in the region [50° W–59° W–5° N–16° N]. Thi...
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ftcopernicus:oai:publications.copernicus.org:bgd98543 2023-05-15T17:31:41+02:00 Impact of North Brazil Current rings on air-sea CO2 flux variability in winter 2020 Olivier, Léa Boutin, Jacqueline Reverdin, Gilles Lefèvre, Nathalie Landschützer, Peter Speich, Sabrina Karstensen, Johannes Ritschel, Markus Wanninkhof, Rik 2021-11-30 application/pdf https://doi.org/10.5194/bg-2021-269 https://bg.copernicus.org/preprints/bg-2021-269/ eng eng doi:10.5194/bg-2021-269 https://bg.copernicus.org/preprints/bg-2021-269/ eISSN: 1726-4189 Text 2021 ftcopernicus https://doi.org/10.5194/bg-2021-269 2021-12-06T17:22:31Z The North Brazil Current (NBC) flows northward across the Equator, passes the mouth of the Amazon River, and forms large oceanic eddies near 8° N. We investigate the processes driving the variability of air-sea CO 2 fluxes at different scales in early 2020 in the region [50° W–59° W–5° N–16° N]. This region is a pathway between the equatorial and North Atlantic Ocean and was surveyed during the EUREC 4 A-OA/ATOMIC campaign. In-situ surface fugacity of CO 2 (fCO 2 ), salinity and temperature combined with maps of satellite salinity, chlorophyll-a and temperature highlight contrasting properties in the region. In February 2020, the area is a CO 2 sink (−1.7 TgC.month −1 ), previously underestimated by a factor 10. The NBC rings transport saline and high fCO 2 water indicative of their equatorial origins and are a small source of CO 2 at regional scale. Their main impact on the variability of biogeochemical parameters is through the filaments they entrain into the open ocean. During the campaign, a nutrient-rich freshwater plume from the Amazon River is entrained from the shelf up to 12° N and caused a phytoplankton bloom leading to a significant carbon drawdown (~20 % of the total sink). On the other hand, saltier filaments of shelf water rich in detrital material act as strong local sources of CO 2 . Spatial distribution of fCO 2 is therefore strongly influenced by ocean dynamics south of 12° N. The less variable North Atlantic subtropical water extends from Barbados northward. They represent ~60 % of the total sink due to their lower temperature associated with winter cooling and strong winds. Text North Atlantic Copernicus Publications: E-Journals |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
The North Brazil Current (NBC) flows northward across the Equator, passes the mouth of the Amazon River, and forms large oceanic eddies near 8° N. We investigate the processes driving the variability of air-sea CO 2 fluxes at different scales in early 2020 in the region [50° W–59° W–5° N–16° N]. This region is a pathway between the equatorial and North Atlantic Ocean and was surveyed during the EUREC 4 A-OA/ATOMIC campaign. In-situ surface fugacity of CO 2 (fCO 2 ), salinity and temperature combined with maps of satellite salinity, chlorophyll-a and temperature highlight contrasting properties in the region. In February 2020, the area is a CO 2 sink (−1.7 TgC.month −1 ), previously underestimated by a factor 10. The NBC rings transport saline and high fCO 2 water indicative of their equatorial origins and are a small source of CO 2 at regional scale. Their main impact on the variability of biogeochemical parameters is through the filaments they entrain into the open ocean. During the campaign, a nutrient-rich freshwater plume from the Amazon River is entrained from the shelf up to 12° N and caused a phytoplankton bloom leading to a significant carbon drawdown (~20 % of the total sink). On the other hand, saltier filaments of shelf water rich in detrital material act as strong local sources of CO 2 . Spatial distribution of fCO 2 is therefore strongly influenced by ocean dynamics south of 12° N. The less variable North Atlantic subtropical water extends from Barbados northward. They represent ~60 % of the total sink due to their lower temperature associated with winter cooling and strong winds. |
format |
Text |
author |
Olivier, Léa Boutin, Jacqueline Reverdin, Gilles Lefèvre, Nathalie Landschützer, Peter Speich, Sabrina Karstensen, Johannes Ritschel, Markus Wanninkhof, Rik |
spellingShingle |
Olivier, Léa Boutin, Jacqueline Reverdin, Gilles Lefèvre, Nathalie Landschützer, Peter Speich, Sabrina Karstensen, Johannes Ritschel, Markus Wanninkhof, Rik Impact of North Brazil Current rings on air-sea CO2 flux variability in winter 2020 |
author_facet |
Olivier, Léa Boutin, Jacqueline Reverdin, Gilles Lefèvre, Nathalie Landschützer, Peter Speich, Sabrina Karstensen, Johannes Ritschel, Markus Wanninkhof, Rik |
author_sort |
Olivier, Léa |
title |
Impact of North Brazil Current rings on air-sea CO2 flux variability in winter 2020 |
title_short |
Impact of North Brazil Current rings on air-sea CO2 flux variability in winter 2020 |
title_full |
Impact of North Brazil Current rings on air-sea CO2 flux variability in winter 2020 |
title_fullStr |
Impact of North Brazil Current rings on air-sea CO2 flux variability in winter 2020 |
title_full_unstemmed |
Impact of North Brazil Current rings on air-sea CO2 flux variability in winter 2020 |
title_sort |
impact of north brazil current rings on air-sea co2 flux variability in winter 2020 |
publishDate |
2021 |
url |
https://doi.org/10.5194/bg-2021-269 https://bg.copernicus.org/preprints/bg-2021-269/ |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
eISSN: 1726-4189 |
op_relation |
doi:10.5194/bg-2021-269 https://bg.copernicus.org/preprints/bg-2021-269/ |
op_doi |
https://doi.org/10.5194/bg-2021-269 |
_version_ |
1766129375793643520 |