Daily Archives: December 5, 2014


angech | December 5, 2014 at 5:07 am | Reply

Willis Eschenbach has an article up at WUWT
Argo And Ocean Heat ContentThe earth is closest to the sun in January, so the earth gains energy around that time, and loses it in the other half of the year. please QUOTE THE EXACT WORDS YOU DISAGREE WITH.

Time for me to get on a hobby horse and get knocked off.

I understand what you are trying to say but disagree with the concept.
The energy in equals the energy out on a 24 hour basis.
Hence when the earth is closer to the sun in January yes there is more energy in but also more energy out to balance.
The atmosphere is naturally hotter as the sun is closer.
But the earth does not retain more energy stored in the sea. Any heat that has gone deep is balanced by colder water elsewhere as the earth has to give up all the energy it takes in over the 24 hour cycle.
If that heat went deep somewhere else had to radiate the equivalent back to space.
Yes there are Kelvin waves, yes, there are pockets of down-welling hot water.
But these do not store extra heat, they only carry heat that has already been balanced by the outgoing radiation from the rest of the sea and land.
That is why “the net TOA imbalance generally only varies by something on the order of ± half a watt per square metre over the thirteen years of the record, with no statistically significant trend at all”
not astounding at all.
TOA is simply the heat in, heat out interface.
Hence so called stored heat cannot come back to bite us. It has already gone back to space.

ENSO and stadium waves and El Nino’s are simply descriptors of current weather patterns.

Yes El Nino is real, the sea is warmer but there is no more heat in the system because of it.

There must be more heat in the system causing El Nino.

The simplest explanation for this would be altered albedo due to cloud cover. This lets more heat into the atmosphere which then heats up.
More complex would be altered albedo due to atmospheric factors we have not taken into account.
Choppy surface water in storms, dust storms, forest fires.
or even factors in the sea which might cause increased reflectance off water.
The last would be simple variance in the amount of energy emitted by the sun which we are reluctant to consider.