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All IPCC definitions taken from Climate Change 2007: The Physical Science Basis. Working Group I Contribution to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Annex I, Glossary, pp. 941-954. Cambridge University Press.

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Archived Rebuttal

This is the archived Intermediate rebuttal to the climate myth "Roy Spencer finds negative feedback". Click here to view the latest rebuttal.

What the science says...

Spencer's model is too simple, excluding important factors like ocean dynamics and treats cloud feedbacks as forcings. A subsequent study by Dessler (2011) found that Spencer's paper was not a test of climate sensitivity or feedbacks, and his assu

Climate scientists have identified a number of fundamental problems in Spencer and Braswell's 2011 study which wrongly concludes that the climate is not sensitive to human greenhouse gas emissions. One of the main problems with the paper is that it uses Roy Spencer's very simple climate model which we've previously looked at in .

Debunked by Trenberth, Fasullo, and Abraham

A commentary published in the same journal (Remote Sensing) by Trenberth, Fasullo, and Abraham found that Spencer's simple model does not have a realistic representation of many key aspects of the Earth's climate system.

"Because the exchange of heat between the ocean and atmosphere is a key part of the ENSO cycle, SB11’s simple model, which has no realistic ocean, no El Niño, and no hydrological cycle, and an inappropriate observational baseline, is unsuitable. Use of a reasonable heat capacity for the ocean is also crucial. Importantly, SB11 treated non-radiative energy exchange between the ocean and atmosphere as a series of random numbers, which neglects the non-random variations of this energy flow associated with the ENSO cycle...None of those processes are included in the SB11 model and its relevance to nature is thus highly suspect."

One key aspect in the Earth's temperature changes is the El Niño Southern Oscillation (ENSO), which is a cycle of the Pacific Ocean. Spencer's model does not include ENSO, and he assumes that ENSO responds to changes in cloud cover, when in reality it's the other way around.

Trenberth et al. found some other key problems in the paper. It doesn't provide enough information for other scientists to repeat the study. However, when trying to replicate their results, Trenberth et al. found that the climate models which matched the observed data best were those with a climate more sensitive to greenhouse gases, which directly contradicts Spencer and Braswell's claims that the climate is not sensitive to greenhouse gases. However, the correlation between model sensitivity and regression strength is of marginal statistical significance. Thus they conclude that Spencer and Braswell fundamentally took the wrong approach:

"Consequently, bounding the response of models by selection of those with large and small sensitivities is inappropriate for these model-observation comparisons."

Trenberth et al. conclude that Spencer and Braswell are not testing climate sensitivity at all, but rather how well climate models simulate El Niño.

It's also worth noting that Remote Sensing does not normally publish climate science research. This may explain how the paper made it through their peer-review system with so many problems. In the end, Trenberth et al. find that the Spencer and Braswell study has no merit.

The model it uses is far too simple to accurately represent the Earth's climate

The paper doesn't provide enough information to replicate their results

Their results depend on using one particular data set

They assume that ENSO responds to cloud cover changes, when in reality, the reverse is true

The study's conclusions are incorrect and unsupportable

Editor-in-Chief Resigns

Wolfgang Wagner, editor-in-chief of the journal which published Spencer's study, has stepped down from his position at Remote Sensing. Wagner concluded the Spencer's paper was "fundamentally flawed and therefore wrongly accepted by the journal". More here...

Debunked by Dessler (2011)

In their paper, Spencer and Braswell analyzed 14 models, but they only plotted the 3 with highest and 3 with lowest equilibrium climate sensitivities. A paper by Dessler (2011) found that in the process, Spencer and Braswell excluded three of the climate model runs which best matched the observational data (Figure 1).

Figure 1: Dessler (2011) reconstruction of Spencer & Braswell's Figure 3, showing relationship between top-of-atmosphere (TOA) net flux and surface temperature, as a function of lag between them. The blue line is the observational data chosen by Spencer and Braswell. The red lines show other available observational data. The black lines show climate model results. The black lines with crosses show the climate model runs chosen by Spencer and Braswell in their paper.

Dessler found that these three model runs excluded by Spencer which best matched the data were also among those which best simulate El Niño and La Niña, which is not surprising, given that much of the temperature change over 2000-2010 was due to the El Niño Southern Oscillation (ENSO). Thus Dessler concludes, like Trenberth et al., that

"since most of the climate variations over this period were due to ENSO, this suggests that the ability to reproduce ENSO is what's being tested here, not anything directly related to equilibrium climate sensitivity."

Spencer's claim of low sensitivity and negative feedbacks is based on this test, which is actually a test of models' ability to reproduce ENSO. Thus Spencer's claim of low sensitivity and negative feedbacks is not supported by the empirical observational data.

Updated on 2012-11-10 by dana1981.

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