>could science fag pleez explain dis.
>30% of the entire delta (Δ) in sea surface temps since 2000, has arrived over merely 3 recent weeks.
>The specific heat content (Q = m * C * ΔT)
Q:heat
m:mass
C: thermal capacity of material (units of energy per unit mass per unit temperature)
ΔT: change in temperature
He's saying that delta-T is too high, relative to the amount of heat transfer that the gaseous atmosphere could impart in 3 weeks. I don't know what he's basing that on.
Usually things like this are due to bad data
Not all delta-T comes from the atmosphere. It comes from radiant heat input also. I don't know how they account for that