Review of Chapter 2, The Hockey Stick Illusion by A. W. Montford
In an attempt to see both sides of the debate in the question of human caused climate change, I am starting to read this book: The Hockey Stick Illusion: Climategate and the Corruption of Science (Independent Minds) by Andrew Montford
As I read it, I will give a chapter by chapter review comprising quotes and commentary. So, if this is an area of interest, keep a watch.
All material quoted from the book is in italics. My comments are in plain text in brackets.
One problem that occurs in
calibration is that any relationship we might have been able to calculate could
have arisen purely by chance. In other words, just because tree ring width
multiplied by ten happened to be equal to temperature in the twentieth century,
that doesn’t mean that it was always that way. For example, twentieth century
ring widths might have been lower than normal, say because of insect
infestation in that particular set of trees, or maybe even in trees in general.
Another possibility is that the tree isn’t actually responding to temperature
at all, but to something else. If any of these issues were really affecting
tree growth, it might be that the normal relationship is actually an extra 0.15
mm of growth from a rise in temperature of 1°C.
[This
is nothing new and climate researchers have already spent considerable effort
addressing the problem. Montford is just grasping at straws here. As just one
example of the ongoing research in this area, see Dendroclimatology: Progress
and Prospects edited by M. K. Hughes, Thomas W. Swetnam, and Henry F. Diaz
(2011)]
If you have a large number of
proxies, there are two main ways in which you can go about the calibration.26
The first of these has been described as ‘the Schweingruber method’, or
composite-plus-scale (CPS), and involves taking proxies that are expected to be
temperature sensitive, calibrating them against local temperatures and essentially
taking an average. The other way, the ‘Fritts method’, or climate field
reconstruction, involves taking lots of proxy series, which are sometimes not
even responding to their local temperatures, and seeing if some sort of
correlation can be found with temperature measurements somewhere in the wider
vicinity. What emerges from this latter method is essentially a weighted
average of the full proxy set, with the temperature sensitive proxies having a
much higher weight than the non-temperature-sensitive ones. It’s this Fritts
method that is the relevant one for our story. The Fritts method involves a
certain leap of faith to trust that trees that are not responding to their own
local temperature can nevertheless detect a signal in a wider temperature index.
You have to believe in the existence of something called ‘teleconnections’,
whereby temperatures in a possibly distant part of the world affect the climate
in the locale of the tree in such a way as to affect its growth, and in a
consistent manner. If this sounds implausible to you, then you are not alone.
However, the reality of the mechanism is accepted by the paleoclimate community
and for the purposes of our story that’s what you need to know.
[Firstly,
The work of Fritts (Tree Rings and Climate, 1976) has stood the test of time
and his methods have been tested and retested by literally hundreds of
scientists. Seems rather arrogant for an armchair climate “expert” to sweep
such work aside so cavalierly. His innuendo concerning the silliness of “teleconnections”
is beyond the pale. Teleconnections are not some hocus pocus. There is more
than a half century of empirical evidence for them, and there are some good
hypotheses about the underlying atmospheric processes. As an example, here is a
quote from The Global Climate System: Patterns, Processes, and Teleconnections
by Howard A. Bridgman and John E. Oliver:
“Teleconnection
is a term used to describe the tendency for atmospheric circulation patterns
to be related, either directly or indirectly, over large and spatially
non-contiguous areas. The AMS Glossary of Weather and Climate (Geer
1996) defined it as a linkage between weather changes occurring in widely
separated regions of the globe. Both definitions emphasize a relationship of
distant processes. However, the word "teleconnection" was not used
in a climate context until it appeared in the mid 1930s (Angstrom 1935), and
even until the 1980s was not a commonly used term in the climatic literature.
“As stressed throughout this book, teleconnections are
often associated with atmospheric oscillations. Any phenomenon that tends to
vary above or below a mean value in some sort of periodic way is properly
designated as an oscillation. If the oscillation has a recognizable
periodicity, then it may be called a cycle, but few atmospheric oscillations
are considered true cycles. This is illustrated by the early problems in
predicting the best-publicized oscillation, the Southern Oscillation and El
NiƱo (Chapter 2). Were this totally predictable then many of its far-reaching
impacts could be forecast.”]
The PCs are often described as
being like the shadow cast by a three-dimensional object. Imagine you are
holding an object, say a comb, up to the sunlight, and it is casting a shadow
on the table in front of you. There are lots of ways you could hold the comb,
each of which would cast a different shadow onto the table, but the one which
tells you the most about the object is when you expose the face of the comb to
the light. When you do this, the sun passes between the teeth and you can see
all the individual points. You can tell from the shadow that what is being held
up is a comb. This shadow is analogous to the first PC. Now rotate the comb
through a right angle, so that you are pointing the long edge of the comb to
the sun. If you do this, the shadow cast is just a long thin line. You can see
from the shadow that you are holding a long thin object, but it could be just
about anything. This would be the second PC. It tells us something about the
object, but not as much as the first PC. You can rotate through a right angle
again and let the sunlight fall on the short edge of the comb. Here the shadow
is almost meaningless. You can tell that something is being held up, but it’s
impossible to draw any meaningful conclusions from it. This then, is the third
PC.
[Montford
spends considerable time in this chapter explaining PCA (Principal Components
Analysis) in lay terms. This is a worthy undertaking, but some of his
description is a bit of an oversimplification. The “shadow” metaphor is a crude
way to explain what PCA results mean. At least he makes some mention of
variance, considering that it is variance that is being partitioned, i.e. what
proportion of the variance can be explained by each component. It also is a bit
annoying for him to abbreviate PCA as just PC, when PCA is the standard
abbreviation used in most publications.]
And that’s it: that’s all you
need to know. Throughout the months and years of bitter argument over Mann’s
Hockey Stick, this simple step was the only part of the PC analysis that was in
dispute. For the purposes of the story it is not really necessary to understand
anything else about how the subsequent calculations work. You can think of PC
analysis as a big black box which takes the centred data and churns out as many
patterns as are felt necessary. It is, however, useful to understand just a
little of the detail of what happens to the centred data, as it will help
explain just why centring is so important.
[This
comes after Montford describes what centering is, a data transformation method
used in the PCA analysis by Mann. What he forgets to point out, is that
although there was a lot of attention paid to this detail of Mann’s analysis,
the results are not even dependent on that approach. More than a dozen
independent analyses since Mann’s first hockey stick, using a variety of
different approaches and data sets, have produced results largely the same. This
seems to be just another example of how climate change contrarians pick some
minor detail that they then consider a fatal defect to the interpretation of
the results.]
P. S.
[I
found a second case of the incorrect use of the word "data" in this
chapter (and more in Chapter 3 which I am now reading), which leads me to
believe that Montford really is not a scientist. I know, I know, some will
accuse me of being nitpicky, but careful analysis and correct writing go hand
in hand in science, and not learning that "data" is a plural word,
and then repeatedly using it as a singular when discussing scientific research
shows a degree of sloppiness and lack of scientific professionalism. Here is
the quote, at any rate:]
"It is important to realise,
however, that this result is only achieved if the data is first centred.
Because of this, centring is considered an integral part of PC analysis."
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