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Spring Phytoplankton Production in the Western Ross Sea
Science, 1994Coastal zone color scanner (CZCS) imagery of the western Ross Sea revealed the presence of an intense phytoplankton bloom covering >106,000 square kilometers in early December 1978. This bloom developed inside the Ross Sea polynya, within 2 weeks of initial polynya formation in late November.
K R, Arrigo, C R, McClain
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The Oceanography and Ecology of the Ross Sea
Annual Review of Marine Science, 2014The continental shelf of the Ross Sea exhibits substantial variations in physical forcing, ice cover, and biological processes on a variety of time and space scales. Its circulation is characterized by advective inputs from the east and exchanges with off-shelf regions via the troughs along the northern portions. Phytoplankton biomass is greater there
Walker O, Smith +3 more
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Albedo of summer snow on sea ice, Ross Sea, Antarctica
Journal of Geophysical Research: Atmospheres, 2007Surface all‐wave albedo and physical parameters (grain radius, mass density, surface temperature, and stratification) of an austral summer snow cover on sea ice were measured in the Ross Sea during January‐February 1999. It was observed that (1) from north to south the snow surface temperature decreases, albedo increases, snow mass density decreases ...
Xiaobing Zhou +3 more
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The ornithology of the Ross Sea
Journal of the Royal Society of New Zealand, 1981Abstract Knowledge of the recent history of antarctic glaciation, sea-ice cover and temperatures suggests that the Ross Sea area has been habitable by birds for some 10,000 years. However, the glaciers in McMurdo Sound precluded colonisation there until about 6,000 yr B.P.
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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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Phylogenetically and functionally diverse microorganisms reside under the Ross Ice Shelf
Nature Communications, 2022Clara Martínez-Pérez +2 more
exaly
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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Long-Term Outcomes of Patients Undergoing the Ross Procedure
Journal of the American College of Cardiology, 2021Martin Andreas +2 more
exaly