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Subinertial Oscillations on the Amundsen Sea Shelf, Antarctica
Wå,hlin, A. K.,Kalé,n, O.,Assmann, K. M.,Darelius, E.,Ha, H. K.,Kim, T. W.,Lee, S. H. AMERICAN METEOROLOGICAL SOCIETY 2016 Journal of physical oceanography Vol.46 No.9
<P>Mooring data from the western flank of Dotson trough, Amundsen Sea shelf region, show the presence of barotropic oscillations with a period of 40-80 h. The oscillations are visible in velocity, temperature, salinity, and pressure and are comparable to tides in magnitude. The period of the oscillations corresponds to topographic Rossby waves of low group velocity and a wavelength of about 40 km, that is, the half-width of the channel. It is suggested that these resonant topographic Rossby waves cause the observed peak in the wave spectra. The observations show that sparseCTDdata from this region should be treated with caution and need to be complemented with moorings or yo-yo stations in order to give a representative picture for the hydrography.</P>
The first report on Amphipoda from Marian Cove, King George Island, Antarctic
Kim, J. H.,JaÅ,¼dÅ,¼ewska, A.,Choi, H. G.,Kim, W. Springer Science and Business Media 2014 Oceanological and hydrobiological studies Vol.43 No.1
This is a first account on amphipods from Marian Cove in Maxwell Bay, near the King Sejong Station, King George Island, the Antarctic. We have conducted a survey in 14 localities in the shallow sublittoral zone. A total of 22 amphipod species belonging to 12 families were identified. Six of these species were new for the whole Maxwell Bay. Our findings increase the amphipod fauna of Maxwell Bay from 55 to 61 species. The dominant species in the shallow sublittoral zone of Marian Cove were: Cheirimedon femoratus and Gondogeneia antarctica, followed by Bovallia gigantea, Orchomenella cf. ultima, Paradexamine fissicauda, Prostebbingia brevicornis, Pariphimedia integricauda, and Jassa wandeli.