Ross Sea Outflow Experiment

Approximately 25% of Antarctic Bottom Water has its origin as dense water exiting the western Ross Sea, but little is known about what controls the release of dense water plumes...约25%的南极底层水（Antarctic Bottom Water）源自流出罗斯海西部的高密度水体，但目前学界对调控此类高密度水羽流释放的具体机制仍知之甚少。