作者: D.R. Turner , N.J.P. Owens
DOI: 10.1016/0967-0645(95)00056-V
关键词:
摘要: Abstract A general overview and background of a two-ship study to examine biogeochemical fluxes in the marginal ice-zone Bellingshausen Sea (65–70°S; 80–87°W), SE Pacific sector Southern Ocean is presented. The major feature studied was an intense band chlorophyll that found geographically close receding ice-edge. However, bloom appeared not be result shallow mixed layer caused by ice-melt stabilisation, but rather associated with oceanic front coincided Details hydrographic conditions existing along 85°W meridian from ice-edge open water north, detailed surveys surface are