Oceanic Heat Content (OHC)

1.   Would it remain feasible to verify and validate the variations in the effective radiative forcings of the earth resulting from enhancement in greenhouse gases and the increase in aerosol concentrations; and also resulting from the variations in Milankovitch cycles (solar activity: eccentricity/obliquity/precession); cirrus clouds (variations in cloud cover reflectivity); albedo effects (variations in snow cover reflectivity) and volcanic changes?

In other words, do we have a clear global energy balance of earth’s climate considering multi-physics having multiple spatial and temporal scales?

2.   Can we precisely estimate the fraction of stored energy in the ocean – between any given specific time-period - from the total energy inflow that remains absorbed within the climate system, given the fact that there is an apparent decadal oscillation in upper-ocean heat storage, along with the presence of biases and uncertainties in OHC resulting from sparse vertical sampling in conjunction with the curvature of the temperature profile with depth?

3.   Was there ocean heat content enhancement prior to 1990?

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