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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Main Authors: Olivier, Léa, Boutin, Jacqueline, Reverdin, Gilles, Lefèvre, Nathalie, Landschützer, Peter, Speich, Sabrina, Karstensen, Johannes, Ritschel, Markus, Wanninkhof, Rik
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/bg-2021-269
https://bg.copernicus.org/preprints/bg-2021-269/
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spelling 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
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id 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
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