Physical factors that affect uptake include increased
ocean stratification due to increasing global temperatures.
When combined with increased
ocean stratification due to this enhanced run off [11], sea - surface temperatures are depressed, encouraging sea - ice formation.
Not exact matches
I understand this is mostly
due to the isostatic pressure being the major factor in the
ocean's density profile resulting in a lot of
stratification.
About half of the pCO2 decrease may be
due to increased glacial
ocean stratification, trapping carbon - rich waters in the deep layers away from the atmosphere (22, 23).
Uncertainty in these projections
due to potential future climate change effects on the
ocean carbon cycle (mainly through changes in temperature,
ocean stratification and marine biological production and re-mineralization; see Box 7.3) are small compared to the direct effect of rising atmospheric CO2 from anthropogenic emissions.
A composite analysis of satellite - based SST measurements reveals that in the tropical region the average strength of the storm - induced sea surface cooling can be explained by the superposition of an effect
due to the storm intensity and an effect associated with the translation speed, and implies that the variability of upper
ocean stratification may not be an important factor in this region
The answer is in thermal expansion of the
ocean waters, which was greater in the early Eocene than in the late Cretaceous,
due to greater temperature
stratification of
ocean water is the early Eocene versus the late Cretaceous.