There's a significant difference between EQUILIBRIUM and TRANSIENT. We are not yet at the equilibrium of the added CO2.
In chemistry if I add two reactants to a mixture they take a certain amount of time to react and then come to equilibrium. Same with added CO2.
RIght now on earth there are a variety of climates. Some hot, some cold, some wet, some dry. Climate change means that
the overall average temperature of the globe can increase while locally climate can cool.
The example I gave of the shutdown of the Thermohaline Circulation in the North Atlantic is a great example. As the globe warms ice on Greenland starts to melt and pump a bunch of fresh water into the upper part of that circulation. The density differential vs salt water can cause the current to slow down or even stop. Right now the climate of England or other western European countries
is warmer than it would normally be at that latitude. That's because the gulf stream pulls warmth up to higher latitudes and that keeps western Europe warmer than it would be without the circulation.
Does that start to make sense? It's a complex system with a lot of moving parts that interact.
You don't have to believe me, you can take the word of actual professional researchers at Columbia University:
In the 2004 disaster movie “The Day After Tomorrow,
news.climate.columbia.edu
The key here is that the ocean is not, even close, to a some static tub of water. It has currents
within it that move up and down and transport north and south and east and west. I was fortunate once to take part in a research cruise in the North Atlantic tracing packets of water as they moved through the ocean water's water column. We were looking at what is called the NADW or North Atlantic Deep Water formation in which water in a "stream" if you will, travels up through the water column, contacts the atmosphere and then cools and sinks to the bottom of the Atlantic and then turns around and rises back up. It's a pretty cool effect but its' basically how the ocean works. It's a complex 3-dimensional system. Not a static bathtub. We were able to find packets of water deep in the Atlantic that contained gases that were human-made in a ratio that existed in the atmosphere maybe 5 or so years ago. Meaning that water was once at the surface.
I did not take a meteorlogy course but I did get to work in the measurement of atmospheric gases interacting with oceans and estuaries.
Which is why I support my points with actual citations.