Not exact matches
As the Atlantic Ocean's
water gets fresher from the melting ice caps, the warm,
saline, and more dense Gulf Stream sinks further south, taking the warmer
water with to the
bottom of the ocean.
Due to the refrigerator effect, cold
saline Antarctic
Bottom Water (proto - AABW) began to dominate the ocean floor.
Contributions of Warm
Saline Deep
Water (WSDW) diminished, and the influential Antarctic Intermediate
Water (AAIW) was increasingly cooled by much colder Antarctic
Bottom Water.