@Article{AvelinaCuFaHaKeMa:2020:InENSA,
author = "Avelina, Raquel and Cunha, Let{\'{\i}}cia Cotrim da and Farias,
C{\'a}ssia de O. and Hamacher, Claudia and Kerr, Rodrigo and
Mata, Maur{\'{\i}}cio M.",
affiliation = "{Universidade do Estado do Rio de Janeiro (UERJ)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Universidade do
Estado do Rio de Janeiro (UERJ)} and {Universidade do Estado do
Rio de Janeiro (UERJ)} and {Brazilian Ocean Acidification Network
(BrOA)} and {Universidade Federal do Rio Grande (FURG)}",
title = "Contrasting dissolved organic carbon concentrations in the
Bransfield Strait, Northern Antarctic Peninsula: insights into
ENSO and SAM effects",
journal = "Journal of Marine Systems",
year = "2020",
volume = "212",
pages = "e103457",
month = "Dec.",
keywords = "Organic matter, Carbon sink, Antarctic water masses, Southern
Ocean, Climate modes.",
abstract = "The marine reservoir of dissolved organic carbon (DOC) is
equivalent to the atmospheric carbon reservoir and represents the
largest reduced carbon stock in the ocean. However, the role of
DOC in the global carbon cycle is not fully understood. In this
study, we analyzed the distribution of DOC in the water column of
the Bransfield Strait, Northern Antarctic Peninsula. Data were
collected during two summer cruises of the NAUTILUS project
conducted by the Brazilian High Latitude Oceanography Group in
February 2015 and 2016. We investigated the possible effects of
the El Nino - Southern Oscillation (ENSO) and Southern Annular
Mode (SAM) climate modes on DOC variability based on correlations
between DOC and temperature, salinity, and dissolved oxygen.
Concentrations of DOC ranged from 40.70 to 122.82 mu mol kg(-1) in
2015 and 33.12 to 112.20 mu mol kg(-1) in 2016. The analysis shows
that the vertical distribution of DOC in the Bransfield Strait may
be controlled by a combination of vertical stratification,
vertical export of organic matter and biological activity in the
upper mixed layer during summertime. The significant interannual
differences observed between DOC concentration and most
physicochemical parameters may be linked to ENSO and SAM climate
modes. The highest DOC concentration was observed in February
2015, associated with a layer of warm surface water, due to the
higher stratification of the water column. The ENSO and SAM
climate modes were low and positive in that year, favoring
intrusions of waters from the Antarctic Circumpolar Current. In
contrast, February 2016 was characterized by record positive ENSO
and SAM modes. The intensification of the Weddell Gyre induced the
advection of cold, more oxygenated and recently formed shelf
waters into the Bransfield Strait, which may have contributed to
the lower DOC concentrations. This study contributes to a better
understanding of the role of DOC in the global carbon cycle in a
region of complex ocean circulation and mixing, and sensitive to
global climate change.",
doi = "10.1016/j.jmarsys.2020.103457",
url = "http://dx.doi.org/10.1016/j.jmarsys.2020.103457",
issn = "0924-7963 and 1879-1573",
language = "en",
targetfile = "avelina_contrasting.pdf",
urlaccessdate = "12 maio 2024"
}