This comes on the heels of last year's record and recent record ocean heat content.
When we combine surface temperatures with ocean heat content, as seen below, a clear picture emerges.
That's how we know that ocean heat content is changing.
Casting characteristics are excellent, since the molten metal has a low heat content and low viscosity.
This is a measure of the required degree of magnetic insulation for the heat content.
In the ocean heat content image above, you might notice a slight change in the trend around 2005.
However, in evaluating the ocean heat content data and scientific literature, Curry made a number of mistakes.
My colleague Dr. Cheng summarized the work by saying, Ocean heat content change is an important metric for the ongoing global warming.
My other colleague, Dr. Lijing Cheng says: Ocean heat content is a vital climate indicator and is a key metric for global warming.
Experts need to beef up ways to measure the heat content of oceans as a way to track more reliably the course of global warming, scientists say today.
Observational evidence from palaeoclimate and of ocean heat content measurements directly contradict the values adopted by M15, but are not acknowledged.
