Results 151 to 160 of about 436,428 (204)

Vertical ocean heat redistribution sustaining sea-ice concentration trends in the Ross Sea. [PDF]

Nat Commun, 2017
Lecomte O, Goosse H, Fichefet T, de Lavergne C, Barthélemy A, Zunz V.   +5 more
europepmc   +1 more source

Increase of the Antarctic Sea Ice Extent is highly significant only in the Ross Sea. [PDF]

Sci Rep, 2017
Yuan N, Ding M, Ludescher J, Bunde A.
europepmc   +1 more source

The paradox of a long grounding during West Antarctic Ice Sheet retreat in Ross Sea. [PDF]

Sci Rep, 2017
Bart PJ, Krogmeier BJ, Bart MP, Tulaczyk S.   +3 more
europepmc   +1 more source

Porifera collection of the Italian National Antarctic Museum (MNA), with an updated checklist from Terra Nova Bay (Ross Sea). [PDF]

Zookeys, 2018
Ghiglione C, Alvaro MC, Cecchetto M, Canese S, Downey R, Guzzi A, Mazzoli C, Piazza P, Rapp HT, Sarà A, Schiaparelli S.   +10 more
europepmc   +1 more source

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Western Ross Sea continental slope gravity currents

Deep Sea Research Part II: Topical Studies in Oceanography, 2009
Antarctic Bottom Water of the world ocean is derived from dense Shelf Water that is carried downslope by gravity currents at specific sites along the Antarctic margins. Data gathered by the AnSlope and CLIMA programs reveal the presence of energetic gravity currents that are formed over the western continental slope of the Ross Sea when High Salinity ...
A. L. GORDON, A. H. ORSI, R. MUENCH, B. A. HUBER, ZAMBIANCHI, Enrico, M. VISBECK   +5 more
openaire   +3 more sources

Fishing for Data in the Ross Sea

Science, 2010
We are among the scientists objecting to the eco-certification of Ross Sea Antarctic toothfish (Dissostichus mawsoni), as described by E. Stokstad in his News Focus story "Behind the eco-label, a debate over Antarctic toothfish" (24 September, p. 1596).
BLIGHT L. K, D. G. AINLEY, S. F. ACKLEY, G. BALLARD, T. BALLERINI, R. L. BROWNELL JR, C. H. CHRISTINA CHENG, CHIANTORE, MARIACHIARA, D. COSTA, M. C. COULTER, P. DAYTON, A. L. DEVRIES, R. DUNBAR, S. EARLE, J. T. EASTMAN, S. D. EMSLIE, C. W. EVANS, R. A. GARROTT, S. KIM, G. KOOYMAN, A. LESCROËL, M. LIZOTTE, M. MASSARO, S. OLMASTRONI, P. J. PONGANIS, J. RUSSELL, D. B. SINIFF, W. O. SMITH JR, B. S. STEWART, I. STIRLING, J. WILLIS, P. WILSON, E. J. WOEHLER   +32 more
openaire   +3 more sources

Picoplankton BIOMASS in the Ross Sea (Antarctica)

Polar Biology, 1993
Spatial distribution of picoplankton in the Ross Sea was studied. The authors discuss the biomasses of various picoplanktonic-sized fractions and of bacterial cells between 0.2 and 2.0 μm capable of growing on Marine Agar 2216 (Difco). Picoplankton having a cellular diameter cf between 1.0 and 2.0 μm (PP1) generally predominate, accounting for 73% of ...
POMAR MLCA, BRUNI V, MAUGERI, Teresa Luciana   +2 more
openaire   +2 more sources

Kerogen Recycling in the Ross Sea, Antarctica

Science, 1974
Analyses of the stable isotopes of the organic carbon and microscopic examination of the sediment particles suggest that up to 90 percent of the organic matter in Ross Sea sediments is derived from the igneous and ancient metamorphic and sedimentary rocks that are being glacially eroded on the Antarctic continent and transported seaward.
W M, Sackett, C W, Poag, B J, Eadie
openaire   +2 more sources

An Apparent Decrease in the Prevalence of "Ross Sea Killer Whales" in the Southern Ross Sea

Aquatic Mammals, 2009
Killer whales (Orcinus orca), both ecotype-B and -C, are important to the Ross Sea, Antarctic ecosystem. The ecotype-C is referred to as “Ross Sea [RS] killer whale.” Herein, we review data on occurrence patterns and diet of RS killer whales and present new information on numbers observed in the southwestern Ross Sea, 2002-2003 to 20082009 austral ...
David G. Ainley, Grant Ballard, Silvia Olmastroni   +2 more
openaire   +2 more sources

Ross Ice Shelf Sea Temperatures

Science, 1979
Two temperature profiles recorded by a sensitive bathythermograph at the Ross Ice Shelf Project site (82°22.5′S, 168°37.5′W) are presented. From the shape of the profiles it is concluded that an inflow of water at intermediate depths provides a source of heat to drive a regime in which ice is melted from the interface at a depth of 360 meters.
openaire   +2 more sources