Physical oceanography and current velocity during Nathaniel B. Palmer cruise NBP97-05

An extensive set of conductivity-temperature-depth (CTD)/lowered acoustic Doppler current profiler (LADCP) data obtained within the northwestern Weddell Sea in August 1997 characterizes the dense water outflow from the Weddell Sea and overflow into the Scotia Sea. Along the outer rim of the Weddell Gyre, there is a stream of relatively low salinity, high oxygen Weddell Sea Deep Water (defined as water between 0° and ?0.7°C), constituting a more ventilated form of this water mass than that found farther within the gyre. Its enhanced ventilation is due to injection of relatively low salinity shelf water found near the northern extreme of Antarctic Peninsula's Weddell Sea shelf, shelf water too buoyant to descend to the deep-sea floor. The more ventilated form of Weddell Sea Deep Water flows northward along the eastern side of the South Orkney Plateau, passing into the Scotia Sea rather than continuing along an eastward path in the northern Weddell Sea. Weddell Sea Bottom Water also exhibits two forms: a low-salinity, better oxygenated component confined to the outer rim of the Weddell Gyre, and a more saline, less oxygenated component observed farther into the gyre. The more saline Weddell Sea Bottom Water is derived from the southwestern Weddell Sea, where high-salinity shelf water is abundant. The less saline Weddell Sea Bottom Water, like the more ventilated Weddell Sea Deep Water, is derived from lower-salinity shelf water at a point farther north along the Antarctic Peninsula. Transports of Weddell Sea Deep and Bottom Water masses crossing 44°W estimated from one LADCP survey are 25 ? 10**6 and 5 ? 10**6 m**3/s, respectively. The low-salinity, better ventilated forms of Weddell Sea Deep and Bottom Water flowing along the outer rim of the Weddell Gyre have the position and depth range that would lead to overflow of the topographic confines of the Weddell Basin, whereas the more saline forms may be forced to recirculate within the Weddell Gyre.

Santa Cruz vista por exploradores y primeros habitantes

Durante la primera mitad del siglo XIX la Patagonia austral argentina permaneció aislada y despoblada; recién en la segunda mitad, autoridades, científicos y pioneros empezaron a ocuparse de ella. A través de este trabajo iremos viendo distintas visiones y experiencias de algunos exploradores y pioneros, tomando como hilo conductor la isla Pavón -negocio de Luis Piedra Buena- y la zona cercana del río Santa Cruz. Esta región era, en esos momentos, la única parte del territorio con algunos habitantes. La factoría de la isla Pavón adquiere no sólo importancia económica, sino particularmente política, frente al desarrollo que va cobrando Punta Arenas y a los deseos del expansionismo chileno. Por esta razón nos detendremos, en un primer momento, en el nacimiento y los años iniciales de este enclave chileno, para comprender la trascendencia que se le debe dar al establecimiento de Piedra Buena, punto hacia donde se dirigía todo explorador y barco argentino y única barrera que existió durante mucho tiempo para defensa de nuestra soberanía.

Relative contents of principal diatom groups in suspended matter and surface layer bottom sediments from the Indian Ocean

Data on relative contents of principal diatom groups in suspended matter collected by a separator on the way of the ship and in bottom sediments from different areas of the Indian Ocean are presented in the paper.