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Our results show that, in general, the increase in glacial freshwater release increases Antarctic sea ice extent.
Two scenarios of glacial freshwater forcing have been designed to account for a decadal perturbation in glacial freshwater release to the Southern Ocean.
The sensitivity of Antarctic sea-ice to increasing glacial freshwater release into the Southern Ocean is studied in a series of 31-year ocean/sea-ice/iceberg model simulations.
For the first time, this perturbation explicitly takes into consideration the spatial distribution of changes in the volume of Antarctic ice shelves, which is found to be a key component of changes in freshwater release.
Our results showed a generally positive effect of freshwater releases, but suggest that adaptive freshwater releases (a long-term, habitat- and species-based freshwater release plan) will be necessary to achieve sustainable wetland biodiversity and improve the efficiency of freshwater utilization.
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The sediment salinity decreased similarly in all three areas after freshwater releases, despite significant differences in salinity before the freshwater releases.
The macrobenthos abundance and biomass generally increased after the freshwater releases, except in the mudflat habitat.
An optimal freshwater releasing time from the upstream reservoir should be chosen at the spring tide.
Trophic state indices classified the lagoons in a bad or poor trophic state most of the year, and they were not able to discriminate the effect of secondary variables such as freshwater releases, ground waters fluxes or water renewal.
Both freshwater releases were performed using truck transport.
The life cycle initiates as eggs are excreted from a mammalian host into freshwater, releasing ciliated, free-swimming larvae called miracidia that seek out and penetrate a snail intermediate host.
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