拉布拉多海

北大西洋热盐环流强度变化对拉布拉多海对流活动的响应，要滞后3a左右。

Response of the North Atlantic thermohaline circulation to the Labrador Sea convection lags 3 years in the model .

在NAO活动达到最强劲状态之后3个月，拉布拉多海对流也达到最深。

Three months after the NAO reaches its maximum state , the Labrador Sea convection reaches its largest depth .

蒸发异常对拉布拉多海表层盐度异常的影响较为显著。

Surface salinity anomalies in the Labrador Sea are created locally by evaporation anomalies at the sinking regions .

20世纪70年代末期开始，格陵兰海、巴伦支海及欧亚大陆大部分区域和北美大陆部分区域在增暖，而拉布拉多海、格陵兰和白令海峡区域却变冷。

From the end of 1970s , the Greenland Sea , the Barents Sea and the most part of Euro-Asian continent and North American continent are getting warmer , whereas the Labrador Sea , the Greenland and the area around the Bering Strait are getting colder .