It seems that those who fear AGW (or at least some of them) do admit that it is not realistic to expect a planetary atmosphere such as ours to warm up oceans of
water over the timescale required by AGW theory because of the huge volume and density of that water and thus the heat storage differentials.
Not exact matches
«This raises the possibility that
water may re-accumulate after extraction, but we need to better understand the physics of why and how this happens to understand the
timescale over which
water may be renewed.»
Basically, although the gas is indeed easily absorbed by sea -
water, it is the
timescales that matter: mixing of shallow and deep oceanic
waters takes place
over hundreds to thousands of years but sea -
water can de-gas parts of its carbon dioxide payload
over much, much shorter periods.
«Evidence indicates that Antarctic bottom
water production through the Holocene (last 10,000 years) is not in a steady - state condition [3], that is to say that bottom
water production sites shift along the Antarctic margin
over decade to century
timescales as conditions for the existence of polynas change.
The main objectives of this study are to better understand the characteristics of the SR through an in - depth assessment of the contemporary
water balance when the basin was intensively monitored (1996 — 2005), to use standardized runoff to select the best
timescale to compute the Standard Precipitation (SPI) and Standard Precipitation Evaporation Indices (SPEI) to estimate trends in
water availability
over 1919 to 2005.
Our study has identified soil
water predictability even beyond the interannual
timescales, thus extending the potential predictive range of hydrological conditions
over North America to almost a decade.
It seemed that the tremendous masses of
water could vary only
over a geological
timescale.
I calculate Delta GT carbon = 6.5 * Delta T + 0.48 * emitted carbon, which I make to convert to 2.8 ppmv per degree C. That's much less than your figure, but given the
timescales one would expect much more outgassing
over a longer period because a greater quantity of
water will warm.
«Based on their results, the researchers conclude that the Arctic Ocean has a previously unrecognized high sensitivity to changes of the freshwater input
over multiple
timescales, which is manifested in large temperature excursions of the intermediate
water layers.»
The pH in surface open - ocean
waters was regulated largely by changes in CO2 because the carbonate ion concentration (CO3 −) concentration is relatively uniform
over the
timescales of interest and ocean
waters are mostly saturated in Ca2 + (Caldeira and Berner 1999).
Basically, although the gas is indeed easily absorbed by sea -
water, it is the
timescales that matter: mixing of shallow and deep oceanic
waters takes place
over hundreds to thousands of years but sea -
water can de-gas parts of its carbon dioxide payload
over much, much shorter periods.
Better climate predictions
over timescales of weeks to decades will help key sectors such as agriculture,
water management, health and energy plan for and adapt to the future.»