It stands to reason that the oceans haven't been that warm in a while but since the average temperature of the whole mass of water is so
dependent on circulation (it's only the surface temperature that's constrained by its interactions with the atmosphere and space), I suppose a plausible history of that particular value would be very hard to reconstruct.
Not exact matches
The Met Office Hadley Centre (Hadley Centre for Climate Prediction and Research) climate change model, Hadley Centre Coupled Model, version 3 (HadCM3)[53], a coupled atmosphere - ocean general
circulation model, was used for the time intervals 2020, 2050 and 2080 (note these date represent a time windows of ten years either side of the time interval date, i.e. 2020 is an average of the years 2010 — 2029, 2050 for 2040 — 2059 and 2080 for 2070 — 2089), under three emission scenarios of the IPCC Special Report
on Emissions Scenarios (SRES)[54]: scenario A1B (maximum energy requirements; emissions differentiated
dependent on fuel sources; balance across sources), A2A (high energy requirements; emissions less than A1 / Fl) and B2A (lower energy requirements; emissions greater than B1).
The exact proportion is model
dependent, and depends
on deep ocean
circulations.
The weakening of the Walker
circulation arises in these models from processes that are fundamentally different from those of El Nià ± o — and is present in both mixed - layer and full - ocean coupled models, so is not
dependent on the models» ability to represent Kelvin waves (by the way, most of the IPCC - AR4 models have sufficient oceanic resolution to represent Kelvin waves and the physics behind them is quite simple — so of all the model deficiencies to focus
on this one seems a little odd).
The flow of energy between different
circulation patterns is
dependent on fram of reference (Eulerian vs transformed Eulerian); The Ferrel Cell is the result of some average upward motion poleward of some average downward motion with return flows at lower and higher altitudes, superimposed
on the average temperature distribution.
The two former methods are
dependent on the large - scale
circulation variables from GCMs, and their value as a viable means of increasing the spatial resolution of climate change information thus partially depends
on the quality of the GCM simulations.
3) That this is a continuous process, so we are really seeing a vertical
circulation, where the original surface water is going to reach an equilibrium T2a (
dependent on turbulence), but which is > T2, and it will eventuall be diplaced upwards as well.
The amount of potential energy released per unit of time is
dependent both
on the rate of the initial evaporation AND the rate of condensation and the net outturn will influence the winds via the pressure gradient and thus the dynamic power of the
circulation.
To confirm that our interpretations are not
dependent on the reanalysis dataset used, we also examined
circulation trends in the ERA - 40 (Uppala et al. 2005) and JRA - 25 (Onogi et al. 2007) reanalysis datasets, and found similar results.
Precipitation is much more
dependent on smaller - scale
circulation and topography.
The bitcoin futures market,
on the other hand, is like an ocean with thermohaline
circulation: its flow is
dependent on several variables.