Not exact matches
There is also a contribution of excess atmospheric CO2 absorption introduced to deep -
water masses from
dense, cold CO2 - rich surface
waters at downwelling sites (e.g., North Atlantic), which then move through the oceans
via meridional overturning circulation.
Cold, polar
waters constantly absorb CO2, sink as it becomes more
dense, and is transported to the equatorial
waters via the ThermoHaline and outgases in the warmer
waters of the Indian and Pacific Oceans.
Dan H.: «Cold, polar
waters constantly absorb CO2, sink as it becomes more
dense, and is transported to the equatorial
waters via the ThermoHaline and outgases in the warmer
waters of the Indian and Pacific Oceans.»
When pulses of warm
water are strong enough to rise over the shelf's outer ridge, that warm
dense water then flows downward to the grounding point of the glacier and remains there until a new equilibrium is established
via basal melting and a retreating grounding point.