Results 1 to 10 of about 14,311 (114)

The role of tides in bottom water export from the western Ross Sea [PDF]

open access: yesScientific Reports, 2021
Approximately 25% of Antarctic Bottom Water has its origin as dense water exiting the western Ross Sea, but little is known about what controls the release of dense water plumes from the Drygalski Trough.
Melissa M. Bowen   +6 more
doaj   +2 more sources

Climatology and decadal variability of the Ross Sea shelf waters

open access: yesAdvances in Oceanography and Limnology, 2011
The World Ocean Database 2001 data located in the Ross Sea (named WOD01 and containing data in this region since 1928) are merged with recent data collected by the Italian expeditions (CLIMA dataset) in the period November 1994-February 2004 in the same ...
A. Russo   +5 more
doaj   +3 more sources

Springtime winds drive Ross Sea ice variability and change in the following autumn [PDF]

open access: yesNature Communications, 2017
Antarctic sea ice extent continues to increase, with autumn sea ice advances in the western Ross Sea particularly anomalous. Here, based on analysis of independent datasets, the authors show that springtime zonal winds in the high latitude South Pacific ...
Marika M. Holland   +3 more
doaj   +2 more sources

Evidence for large-scale climate forcing of dense shelf water variability in the Ross Sea [PDF]

open access: yesNature Communications
Antarctic Bottom Water (AABW), which supplies the lower limb of the thermohaline circulation, originates from dense shelf water (DSW) forming in Antarctic polynyas.
Zhaoru Zhang   +11 more
doaj   +2 more sources

Rebound of shelf water salinity in the Ross Sea [PDF]

open access: yesNature Communications, 2019
Ross Sea Bottom Water, a major source of Antarctic Bottom Water, has experienced significant freshening in recent decades. Here the authors use 23 years of summer measurements to document temporal variability in the salinity of the Ross Sea High Salinity
Pasquale Castagno   +7 more
doaj   +2 more sources

Cold call: the acoustic repertoire of Ross Sea killer whales (Orcinus orca, Type C) in McMurdo Sound, Antarctica [PDF]

open access: yesRoyal Society Open Science, 2020
Killer whales (Orcinus orca) are top marine predators occurring globally. In Antarctic waters, five ecotypes have been described, with Type C being the smallest form of killer whale known.
Rebecca Wellard   +3 more
doaj   +2 more sources

Tintinnid ciliates (marine microzooplankton) of the Ross Sea

open access: yesPolar Research, 2022
For the Ross Sea, the only Marine Protected Area in Antarctica, available data on the tintinnid ciliates of the marine microzooplankton are mostly limited to nearshore waters near Terra Nova Bay or the vicinity of the McMurdo Sound.
John R. Dolan   +4 more
doaj   +1 more source

The Ross Sea Dipole – temperature, snow accumulation and sea ice variability in the Ross Sea region, Antarctica, over the past 2700 years [PDF]

open access: yesClimate of the Past, 2018
High-resolution, well-dated climate archives provide an opportunity to investigate the dynamic interactions of climate patterns relevant for future projections. Here, we present data from a new, annually dated ice core record from the eastern Ross Sea,
N. A. N. Bertler   +87 more
doaj   +1 more source

Past ice-sheet behaviour: retreat scenarios and changing controls in the Ross Sea, Antarctica [PDF]

open access: yesThe Cryosphere, 2016
Studying the history of ice-sheet behaviour in the Ross Sea, Antarctica's largest drainage basin can improve our understanding of patterns and controls on marine-based ice-sheet dynamics and provide constraints for numerical ice-sheet models.
A. R. W. Halberstadt   +3 more
doaj   +1 more source

Carbonate saturation state of surface waters in the Ross Sea and Southern Ocean: controls and implications for the onset of aragonite undersaturation [PDF]

open access: yesBiogeosciences, 2015
Predicting when surface waters of the Ross Sea and Southern Ocean will become undersaturated with respect to biogenic carbonate minerals is challenging in part due to the lack of baseline high-resolution carbon system data. Here we present ~ 1700 surface
H. B. DeJong   +3 more
doaj   +1 more source

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