Deep thermohaline Circulation in the low-latitude Atlantic during the Last Glacial
Present-day low-latitude eastern and western Atlantic basins are geochemically distinct below the sill depth of the Mid-Atlantic Ridge. While Antarctic Bottom Water (AABW) circulates freely in the western Atlantic, flow into the eastern Atlantic is restricted below 4 km which results in filling the...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1995
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.692007 https://doi.org/10.1594/PANGAEA.692007 |