The mechanism by which the effect of
oceanic variability over time is transferred to the atmosphere involves evaporation, conduction, convection, clouds and rainfall the significance of which has to date been almost entirely ignored due to the absence of the necessary data especially as regards the effect of cloudiness changes on global albedo and thus the amount of solar energy able to enter the oceans.
Not exact matches
«Even if it (the solar effect) is only 0.1 C
over a solar cycle and a little more
over a 500 year period from LIA to date then that's a good enough starting point for my NCM because all such solar
variability needs to do is alter the size, position and intensity of the polar high pressure cells against an opposing force from
oceanic variability.
Even if it is only 0.1 C
over a solar cycle and a little more
over a 500 year period from LIA to date then that's a good enough starting point for my NCM because all such solar
variability needs to do is alter the size, position and intensity of the polar high pressure cells against an opposing force from
oceanic variability.