论文部分内容阅读
自50年代后期以来国际上对普里兹湾区海洋过程的调查研究不断加强(Zverev,1959,1963;Izvekov,1959),尤其是进入80年代后,由于在现场考察中采用了CTD系统和浮标测流系统,人们对该区海洋过程的认识有了长足的进步。但由于该海区的热盐结构有非常显著的时空变化(Kornilov,1971;Smith et al.,1984;Middleton and Hamphries,1989;乐肯堂等,1996,1997),因而对该海区水团和环流中的若干重要问题,例如
Since the late 1950s, there has been an increasing international investigation into the ocean processes in the Prydz Bay (Zverev, 1959, 1963; Izvekov, 1959). Especially since the 1980s, CTD systems and buoys have been used in field missions Current-measuring system, people have made great progress in the understanding of the marine processes in the area. However, due to the very significant temporal and spatial variations of the thermohaline structure in the sea area (Kornilov, 1971; Smith et al., 1984; Middleton and Hamphries, 1989; Leken Hall et al., 1996, 1997) A number of important issues, for example