Variations in the summer oceanic p CO 2 and carbon sink in Prydz Bay using the self-organizing map analysis approach
2019
Abstract. This study applies a neural network technique to produce maps
of oceanic surface p CO 2 in Prydz Bay in the Southern
Ocean on a weekly 0.1 ∘ longitude × 0.1 ∘ latitude
grid based on in situ measurements obtained during the 31st CHINARE cruise
from February to early March 2015. This study area was divided into three
regions, namely, the “open-ocean” region, “sea-ice” region and “shelf” region. The
distribution of oceanic p CO 2 was mainly affected by
physical processes in the open-ocean region, where mixing and upwelling were
the main controls. In the sea-ice region, oceanic p CO 2
changed sharply due to the strong change in seasonal ice. In the shelf
region, biological factors were the main control. The weekly oceanic
p CO 2 was estimated using a self-organizing map (SOM) with
four proxy parameters (sea surface temperature, chlorophyll a
concentration, mixed Layer Depth and sea surface salinity) to overcome the
complex relationship between the biogeochemical and physical conditions in
the Prydz Bay region. The reconstructed oceanic p CO 2 data
coincide well with the in situ p CO 2 data from
SOCAT, with a root mean square error of 22.14 µ atm. Prydz Bay
was mainly a strong CO 2 sink in February 2015, with a monthly
averaged uptake of 23.57±6.36 TgC. The oceanic CO 2 sink is
pronounced in the shelf region due to its low oceanic
p CO 2 values and peak biological production.
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