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Marine Protection in the Ross Sea
2011Lincoln Planning Review, Vol 3, No 1 (2011)
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Phenolic compounds in Ross Sea water
2016Phenolic compounds are semi-volatile organic compounds produced during biomass burning and lignin degradation in water. In atmospheric and paleoclimatic ice cores studies, these compounds are used as biomarkers of wood combustion and supply information on the type of combusted biomass.
Zangrando Roberta +6 more
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The Odyssea Drift (Ross Sea, Antarctica).
2018The Hillary Canyon is one of the main conduits for dense shelf water forming in the Ross Sea, which over-flows the shelf edge and transforms into the Antarctic Bottom Water (AABW). The main changes in past ocean circulation are recorded in the adjacent ODYSSEA Contourite Depositional System that is located at 2000-3000 m depth west of the Hillary ...
Rebesco M. +25 more
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Sea bottom morphologies of the Ross Sea area (Antarctica)
1993During the 1987-88, 1988-89, 1989-90 and 1990-91 Austral summers, multichannel seismic reflection, gravity and magmatic surveys in the Ross Sea were recorded and then processed by the Osservatorio Geofisico Sperimentale (OGS) of Trieste. Some of the most evident morphological features of the sea bottom in the Ross Sea and their spatial distribution are
Marchetti A +5 more
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Spectrum and Outcome of Reoperations After the Ross Procedure
Circulation, 2010Hartzell V Schaff
exaly

