拉布拉多寒流
- 网络Labrador Current;LabradorColdCurrent
拉布拉多寒流-
LGM时期墨西哥湾暖流和北大西洋暖流的减弱以及拉布拉多寒流的增强，使得向北热量传输的减少，从而导致了SST的剧烈下降，同时也导致了海冰的扩展。
The weaker Gulf Stream and North Atlantic Drift and stronger Labrador Current during LGM could lead to the decrease in oceanic northward heat transport , resulting in the strong cooling of the SST and the increase in the sea ice concentration .
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北上的墨西哥湾暖流与南下的拉布拉多寒流，在新英格兰海岸的附近相遇。
The warm Guff Stream sweeping north and the frigid Labrador Current flowing south meet just off the New England coast .