Tropical cooling at the last glacial maximum and extratropical ocean ventilation<cross-ref refid="fnote01" type="ftnote">1</cross-ref><ftnote id="fnote01"><p id="spara1">CCR contribution number: 780.</p></ftnote>

Physics

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Global Change: Climate Dynamics (3309), Global Change: Oceans (4203), Oceanography: General: Paleoceanography, Meteorology And Atmospheric Dynamics: Paleoclimatology

Scientific paper

The NCAR CSM is used to simulate the climate at Last Glacial Maximum.
The CSM simulates a tropical SST cooling of 2.1°C. It is shown that
about half of this tropical cooling is associated with the upper ocean
circulation, especially the ventilation of thermocline and intermediate
waters from the mid/high latitude South Pacific.

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Tropical cooling at the last glacial maximum and extratropical ocean ventilation<cross-ref refid="fnote01" type="ftnote">1</cross-ref><ftnote id="fnote01"><p id="spara1">CCR contribution number: 780.</p></ftnote> does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

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