Sunday, April 15, 2007

The speakable and unspeakable in climate science


There is a wonderful monograph by the late John Bell, The Speakable and Unspeakable in Quantum Mechanics which deals with the issue of what can and cannot be described on many levels. Roger Pielke Sr. is pursuing such a chimera, demanding that we use metrics of climate change which are simply either not available, or available only for short periods of time, or, as we have seen for ocean heat content, or are not (one hopes yet) reliable.

Now, Roger Pielke Senior is a fan of the IPCC using such metrics such as “the global-averaged and regional-averaged patterns of changes in heat content in units of Joules” instead of surface temperatures. Eli wished him great good luck in explaining that to your average policy maker.

Well, how about enthalpy or energy content. Eli agrees, the perfect measure would be the energy change of the oceans, surface and atmosphere. One could settle for lower atmosphere and upper ocean. Multidecadal records of these too are not currently available and, as yesterday's post shows, many of the measurements that we have are not as good as we would wish. Worse from the standpoint of Pielke, the best way of reconstructing such profiles is through models which can be validated by comparison with the data we do have, such as records of surface temperatures and precipitation.

To paraphrase Thomas Knutson: Should we use surface temperature observations or energy content profiles? In reply we note that if we had multidecadal observations of energy content throughout the oceans and atmosphere, we obviously would trust them more than the surface temperature records, but unfortunately we cannot go back in time with modern instrumentation and recapture the needed profiles.

Eli wishes to emphasize that the only way to get those profiles is through inproved postdiction with models. Those who demand unknowable perfection before doing anything have little interest in action. They don't much like proxy measurements either.

Yesterday, when describing a few of the problems with ocean heat content measurements, Eli forgot to point to this post by Tamino which showed that even without corrections, the differences between the models and the observations were within natural variability. The figure is from Hansen et al. (2005, Science, vol. 308, pg. 1431).


It will be interesting to replot the models against corrected observations.

6 comments:

  1. According to the graph on the Argo Information center site, ocean heat content peaked in 2003 followed by a decrease of about 1 W/m^2 for the years through 2005.

    "Oceanographers have detected a new cooling event that began in 2003, following 8 years of warming, using satellite and in-situ data."

    It appears from this NASA presentation Ocean Heat Storage and Net Radiation: Cooling? Ocean Heat Storage and Net Radiation: Cooling?that the cooling has not yet been explained.

    ReplyDelete
  2. Per discussion elsewhere, the ARGO results showing cooling have been erased. The remaining ARGO data now appears to be very consistent with the satellite TOA results as reported in the link (i.e., essentially flat for the last two years), although in the end GRACE will tell.

    ReplyDelete
  3. Steve,

    How is it that the cooling effect was "erased"?

    Do you have the link to that?

    ReplyDelete
  4. I guess you're new here -- see the immediate prior post on this very blog.

    ReplyDelete
  5. Of course, talking to a decision-maker with phrases like global-averaged and regional-averaged patterns of changes in heat content in units of Joules would serve to delay action another few years...

    Taking this tactic, though, seems to be a non-starter for poor RPSr.

    Best,

    D

    ReplyDelete

Dear Anonymous,

UPDATE: The spambots got clever so the verification is back. Apologies

Some of the regulars here are having trouble telling the anonymice apart. Please add some distinguishing name to your comment such as Mickey, Minnie, Mighty, or Fred.

You can stretch the comment box for more space

The management.