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Continuous winter oceanic profiling in the Cape Darnley Polynya, East Antarctica
by
Ono, Kazuya
, Aoki, Shigeru
, Hirano, Daisuke
, Tamura, Takeshi
in
Abyssal environment
/ Capes (landforms)
/ Dense water
/ Earth and Environmental Science
/ Earth Sciences
/ Freshwater & Marine Ecology
/ Oceanography
/ Original Article
/ Polynyas
/ Profiles
/ Salinity
/ Salinity effects
/ Salinity profiles
/ Sea ice
/ Stratification
/ Vertical distribution
/ Vertical mixing
/ Water circulation
/ Water column
/ Winter
2020
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Continuous winter oceanic profiling in the Cape Darnley Polynya, East Antarctica
by
Ono, Kazuya
, Aoki, Shigeru
, Hirano, Daisuke
, Tamura, Takeshi
in
Abyssal environment
/ Capes (landforms)
/ Dense water
/ Earth and Environmental Science
/ Earth Sciences
/ Freshwater & Marine Ecology
/ Oceanography
/ Original Article
/ Polynyas
/ Profiles
/ Salinity
/ Salinity effects
/ Salinity profiles
/ Sea ice
/ Stratification
/ Vertical distribution
/ Vertical mixing
/ Water circulation
/ Water column
/ Winter
2020
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Continuous winter oceanic profiling in the Cape Darnley Polynya, East Antarctica
by
Ono, Kazuya
, Aoki, Shigeru
, Hirano, Daisuke
, Tamura, Takeshi
in
Abyssal environment
/ Capes (landforms)
/ Dense water
/ Earth and Environmental Science
/ Earth Sciences
/ Freshwater & Marine Ecology
/ Oceanography
/ Original Article
/ Polynyas
/ Profiles
/ Salinity
/ Salinity effects
/ Salinity profiles
/ Sea ice
/ Stratification
/ Vertical distribution
/ Vertical mixing
/ Water circulation
/ Water column
/ Winter
2020
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Continuous winter oceanic profiling in the Cape Darnley Polynya, East Antarctica
Journal Article
Continuous winter oceanic profiling in the Cape Darnley Polynya, East Antarctica
2020
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Overview
Antarctic coastal polynyas provide extremely dense water to the global abyss, but the dense water formation process has been poorly monitored in winter. This study developed a new tethered profiler to realize time-series observations of the water column in the Cape Darnley Polynya, East Antarctica. The system successfully obtained temperature and salinity profiles at 10-day intervals from March to November 2017. From March to April, significant cooling and vertical mixing started, while stratification collapsed. Salinity increased rapidly from April to late-May and then gradually increased until October. Salinity development was largely consistent with the cumulative salt increase due to sea-ice production at the initial stage, but not at latter stages, indicating the influence of cross-shelf exchange. These results highlighted the potential of the measurement platform to fill the remaining gap in the global ocean monitoring network.
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