I have to keep stressing that the ocean has currents which also run up and down in the water column. It transfers heat not just through passive convection through standing water.
I thought I'd made that clear with the discussion of the NADW.
Oceanolography isn't your strong suit I guess ... from
Vedantu Learning Center: ...
"Oceanic circulation can be divided into two kinds: wind-driven circulation and thermohaline circulation. Wind-driven circulation involves the horizontal movement of surface seawater with the help of wind current and it generates large gyres on the ocean. In contrast, thermohaline circulation is much sluggish and involves the vertical movement of seawater predominantly.
It is observed that such circulation has a typical speed of 1 centimetre per second but it involves a movement of huge amounts of water that carries heat, salts and other nutrients of seawater."
... [Emphasis mine]
So ... thermohaline current is 0.01 m/s ... Gulf Stream is 2 m/s ... are you still having basic arithmetic issues? ... which one of these carries 200 times the power ... ha ha ha ha ha ha ...
"Temperature and salinity are the main driving force of such circulation of seawater. During the winter season, the surface water becomes denser due to cooling and net evaporation that is why it sinks to the deeper region of the ocean and spreads slowly. Seawater at depth replaces the surface water that sinks. That is how the thermohaline circulation takes place."
I am glad you brought this up ... I was wrong about the mechanism ... but my argument still stands... "just in winter, that'll turn your annual average to garbage?" ...
A good local example of this is the outflow of the Mediterranean ... so much water is evaporating off the surface that the water is much more salty as it leaves ... research shows this denser water flows "downhill" just like a river to the ocean abyss ... just not enough mass to carry much energy ... and it too is very slow ...
God ... look at the map ... this isn't in the oceans ... it's in the Atlantic ... and that's not a real ocean ... I'm from the
Best West Coast, so I know better ... that's driving your global averages down down down ... too much of the oceans aren't subject as much to this current ...
The only thing you made clear is that you don't know very much about the NADW ...
ETA: [Later] ... that should read "vertical convection" ... my apologies ... horizontal convection would NOT be inhibited by this mechanic ...
The math works out. Because it includes details about how ocean circulation actually works.
Not even close. You are talking straight convection in a standing body of water. That couldn't be FURTHER AWAY from what the ocean is like.
There is a temperature inversion in the oceans ... as we are heating the oceans from the top ... this top layer of water is the least dense, thus most buoyant ... and will stay at the top ...
inhibiting convection ...
Just so we're clear ... the short wave energy is deposited in the top 1 meter of the ocean ... making that layer "hot" with respect to the layer below it and also the atmosphere above it ... here the 2nd Law requires energy to leave this top layer, and to leave through any means possible, up or down ... proportional to the force driving the energy ... you do remember what "work performed" is, don't you? ... we can't convect down the water column, but we sure as hell can convect up the air column ... same with radiation ...
If you're conducting the energy down ... then you're not irradiating carbon dioxide in the atmosphere .. now are you? ... think "1st Law"
"1st Law" "1st Law" "1st Law"