The Elusive ~ 60-year Sea Level Cycle

Guest Post by Willis Eschenbach

I was referred to a paywalled paper called “Is there a 60-year oscillation in global mean sea level?”  The authors’ answer to the eponymous question is “yes”, in fact, their answer boils down to “dangbetcha fer sure yes there is a 60-year oscillation”, viz:

We examine long tide gauge records in every ocean basin to examine whether a quasi 60-year oscillation observed in global mean sea level (GMSL) reconstructions reflects a true global oscillation, or an artifact associated with a small number of gauges. We find that there is a significant oscillation with a period around 60-years in the majority of the tide gauges examined during the 20th Century, and that it appears in every ocean basin.

So, as is my wont, to investigate this claim I got data. I went to the PSMSL, the Permanent Service for the Mean Sea Level, and downloaded all their monthly tidal records, a total of 1413 individual records. Now, the authors of the 60-year oscillation paper said they looked at the “long-term tide records”. If we’re looking for a 60-year signal, my rule of thumb says that you need three times that, 180 years of data, to place any confidence in the results. Bad news … it turns out only two of the 1,413 tidal gauge records, Brest and Swinoujscie, have 180 years of data. So, we’ll need to look at shorter records, maybe a minimum of two times the 60-year cycle we’re looking for. It’s sketchy to use that short of a record, but “needs must when the devil drives”, as the saying goes. There are twenty-two tidal datasets with 120 years or more of data. Figure 1a shows the first eight of them:

all tide records over 120 years 1-8Figure 1a. Tide gauge records with 1440 months (120 years) or more of records. These are all relative sea levels, meaning they are each set to an arbitrary baseline. Units are millimetres. Note that the scales are different, so the trends are not as uniform as they appear.

Now, there’s certainly no obvious 60-year cycles in those tidal records. But perhaps the subtleties are not visible at this scale. So the following figure shows the Gaussian averages of the same 8 tidal datasets. In order to reveal the underlying small changes in the average values, I have first detrended each of the datasets by removing any linear trend. So Figure 1b emphasizes any cycles regardless of size, and as a result you need to note the very different scales between the two figures 1a and 1b.

gauss all tide records over 120 years 1-8Figure 1b. Gaussian averages (14-year full-width half-maximum) of the linearly detrended eight tide gauge datasets shown in Figure 1a. Note the individual scales are different from Figure 1a.

Huh. Well, once the data is linearly detrended, we end up with all kinds of swings. The decadal swings are mostly on the order of 20-30 mm (one inch) peak to peak, although some are up to about twice that. The big problem is that the decadal swings don’t line up, they aren’t regular, and they don’t have any common shape. More to the current point, there certainly is no obvious 60-year cycle in any of those datasets.

Now, we can take a closer look at what underlying cycles are in each of those datasets by doing a periodicity analysis. (See the notes at the end for an explanation of periodicity analysis). It shows how much power there is in the various cycle lengths, in this case from two months to seventy years Figure 1c shows the periodicity analysis of the same eight long datasets. In each case, I’ve removed the seasonal (annual) variations in sea level before the periodicity analysis.

periodicity all tide records over 120 years 1-8Figure 1c. Periodicity analysis, first eight long-term tidal datasets.

Boooring … not much of anything anywhere. Top left one, Brest, has hints of about a 38-year cycle. New York shows a slight peak at about 48 years. Other than that there is no energy in the longer-term cycles, from say 30 to 70 years.

So let’s look at the rest of the 22 datasets. Here are the next eight tide gauge records, in the same order—first the raw record, then the Gaussian average, and finally the periodicity analysis.

all tide records over 120 years 9-16 gauss all tide records over 120 years 9-16 periodicity all tide records over 120 years 9-16Figures 2a, 2b, and 2c. Raw data, Gaussian averages, and periodicity analysis, next 8 stations longer than 120 years.

No joy. Same problem. All kinds of cycles, but none are regular. The largest problem is the same as in the first eight datasets—the cycles are irregular, and in addition they don’t line up with each other. Other than a small peak in Vlissingen at about 45 years, there is very little power in any of the longer cycles. Onwards. Here are the last six of the twenty-two 120-year or longer datasets:

all tide records over 120 years 17-22 gauss all tide records over 120 years 17-22 periodicity all tide records over 120 years 17-22

Figures 3a, 3b, and 3c. Data, Gaussian averages, and periodicity analysis as above, for the final six 120-year + tide gauge datasets. 

Dang, falling relative sea levels in Figure 3a. Obviously, we’re looking at some tidal records from areas with “post-glacial rebound” (PGR), meaning the land is still uplifting after the removal of trillions of tons of ice at the end of the last ice age. As a result, the land is rising faster than the ocean …

How bizarre. I just realized that people worry about sea-level rise as a result of global warming, and here, we have land-level rise as a result of global warming  … but I digress. The net result of the PGR in certain areas are the falling relative sea levels in four of the six datasets.

Like the other datasets, there are plenty of cycles of various kinds in these last six datasets in Figure 3, but as before, they don’t line up and they’re not regular. Only two of them have something in the way of power in the longer cycles. Marseille has a bit of power in the 40-year area. And dang, look at that … Poti, the top left dataset, actually has hints of a 60-year cycle … not much, but of the twenty-two datasets, that’s the only one with even a hint of power in the sixty-year range.

And that’s it. That’s all the datasets we have that are at least twice as long as the 60-year cycle we’re looking for. And we’ve seen basically no sign of any significant 60-year cycle.

Now, I suppose I could keep digging. However, all that are left are shorter datasets … and I’m sorry, but looking for a sixty-year cycle in a 90-year dataset just isn’t science on my planet. You can’t claim a cycle exists from only enough data to show one and a half swings of the cycle. That’s just wishful thinking. I don’t even like using just two cycles of data, I prefer three cycles, but two cycles is the best we’ve got.

Finally, you might ask, is it possible that if we average all of these 22 datasets together we might uncover the mystery 66-year cycle? Oh, man, I suppose so, I’d hoped you wouldn’t ask that. But looking at the mish-mash of those records shown above, would you believe it even if I found such a cycle? I don’t even like to think of it.

Ah, well, for my sins I’m a scientist, I am tormented by unanswered questions. I’d hoped to avoid it, so I’ve ignored it up until now, but hang on, let me do it. I plan to take the twenty-two long-term records, linearly detrend them, average them, and show the three graphs (raw data, Gaussian average, and periodicity analysis) as before. It’ll be a moment.

OK. Here we go. First the average of all of the detrended records, with the Gaussian average overlaid.

mean detrended 22 tide recordsFigure 4a. Mean of the detrended long-term tidal records. Red line shows a 14-year full-width half-maximum (FWHM) Gaussian average of the data, as was used in the earlier Figures 1b, 2b, 3b.

Well, I’m not seeing anything in the way of a 60-year cycle in there. Here’s the periodicity analysis of the same 22-station mean data:

periodicity mean detrended 22 tide recordsFigure 4b. Periodicity analysis of the data shown in Figure 4a immediately above.

Not much there at all. A very weak peak at about forty-five years that we saw in some of the individual records is the only long-term cycle I see in there at all.

Conclusions? Well, I don’t find the sixty-year cycle that they talk about, either in the individual or the mean data. In fact, I find very little in the way of any longer-term cycles at all in the tidal data. (Nor do I find cycles at around eleven years in step with the sunspots as some folks claim, although that’s a different question.) Remember that the authors said:

We find that there is a significant oscillation with a period around 60-years in the majority of the tide gauges examined during the 20th Century …

Not able to locate it, sorry. There are decadal swings of about 25 – 50 mm (an inch or two) in the individual tide gauge datasets.  I suppose you could call that “significant oscillations in the majority of the tide gauges”, although it’s a bit of a stretch.

But the “significant oscillations” aren’t regular. Look at the Gaussian averages in the first three sets of figures. The “significant oscillations” are all over the map. To start with, even within each individual record the swings vary greatly in amplitude and cycle length. So the cycles in each individual record don’t even agree with themselves.

Nor do they agree with each other. The swings in the various tidal records don’t line up in time, nor do they agree in amplitude.

And more to the point, none of them contain any strong approximately sixty-year signal. Only one of the twenty-two (Poti, top left in Figure 3a,b,c) shows any power at all in the ~ 60 year region in the periodicity analysis.

So I’m saying I can’t find any sign in those twenty-two long tidal datasets of any such sixty-year cycle. Note that this is different from saying that no such cycle exists in the datasets. I’m saying that I’ve pulled each one of them apart and examined them individually as best I know how, and I’m unable to find the claimed “significant oscillation with a period around 60-years” in any of them.

So I’m tossing the question over to you. For your ease in analyzing the data, which I obtained from the PSMSL as 1413 individual text files, I’ve collated the 1413 record tide station data into a 13 Mb Excel worksheet, and the 22 long-term tidal records into a much smaller CSV file. I link to those files below, and I invite you to try your hand at demonstrating the existence of the putative 60-year cycle in the 22-station long-term tidal data.

Some folks don’t seem to like my use of periodicity analysis, so please, use Fourier analysis, wavelet analysis, spectrum analysis, or whatever type of analysis you prefer to see if you can establish the existence of the putative “significant” 60-year cycles in any of those long-term tidal datasets.

Regards to all, and best of luck with the search,

w.

The Standard Request: If you disagree with something someone says, please have the courtesy to quote the exact words you disagree with. It avoids all kinds of trouble when everyone is clear what you are objecting to.

Periodicity Analysis: See the post “Solar Periodicity” and the included citations at the end of that post for a discussion of periodicity analysis, including an IEEE Transactions paper containing a full mathematical derivation of the process.

Data: I’ve taken all of the PSMSL data from the 1413 tidal stations and collated it into a single 13.3 Mb Excel worksheet here. However, for those who would like a more manageable spreadsheet, the 22 long-term datasets are here as a 325 kb comma-separated value (CSV) file.

[UPDATE] An alert commenter spots the following:

Jan Kjetil Andersen says:

April 26, 2014 at 2:38 pm

By Googling the title I found the article free on the internet here:

http://www.nc-20.com/pdf/2012GL052885.pdf

I don’t find it any convincing at all. They use the shorter series in the PSMSL sets, and claim to see 64 years oscillations even though the series are only 110 years long.

The article has no Fourier or periodicity analysis of the series.

/Jan

Thanks much for that, Jan. I just took a look at the paper. They are using annually averaged data … a very curious choice. Why would you use annual data when the underlying PSMSL dataset is monthly?

In any case, the problem with their analysis is that you can fit a sinusoidal curve to any period length in the tidal dataset and get a non-zero answer. As a result, their method (fit a 55 year sine wave to the data) is meaninglesswithout something with which to compare the results.

A bit of investigation, for example, gives the following result. I’ve used their method, of fitting a sinusoidal cycle to the data. Here are the results for Cascais, record #43. In their paper they give the amplitude (peak to peak as it turns out) of the fitted sine curve as being 22.3. I get an answer close to this, which likely comes from a slight difference in the optimization program.

First, let me show you the data they are using:

If anyone thinks they can extract an “~ 60 year” cycle from that, I fear for their sanity …

Not only that, but after all of their waffling on about an “approximately sixty year cycle”, they actually analyze for a 55-year cycle. Isn’t that false advertising?

Next, here are the results from their sine wave type of analysis analysis for the periods from 20 to 80 years. The following graph shows the P-P amplitude of the fitted sine wave at each period.

So yes, there is indeed a sinusoidal cycle of about the size they refer to at 55 years … but it is no different from the periods on either side of it. As such, it is meaningless.

The real problem is that when the cycle length gets that long compared to the data, the answers get very, very vague … they have less than a hundred years of data and they are looking for a 55-year cycle. Pitiful, in my opinion, not to mention impossible.

In any case, this analysis shows that their method (fit a 55-year sine wave to the data and report the amplitude) is absolutely useless because it doesn’t tell us anything about the relative strength of the cycles.

Which, of course, explains why they think they’ve found such a cycle … their method is nonsense.

Eternal thanks to Jan for finding the original document, turns out it is worse than I thought.

w.

 

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Greg
April 30, 2014 2:49 pm

Bart : “Yes, it is very clear that the approximately 10, 10.8, 11.8, and 134 year components evident in the SSN data are coming from rectification of processes centered at approximately 20 and 23.6 years.”
Could you elaborate ? Link ?
thx

Latitude
April 30, 2014 2:53 pm

Don’t want to interrupt….just thank you guys for giving us/me an incredible education

1sky1
April 30, 2014 6:46 pm

Willis:
There you go ad hominem again, with your put or shut up meme! Meanwhile, you
remain clueless as to what’s involved in analyzing tidal data for major
constituents. You need HOURLY data for at least a month for LS analysis
(see http://drs.nio.org/drs/bitstream/2264/59/4/Mahasagar_24_1.pdf). And
for a fuller set of tidal constituents, in accordance with Doodson’s
time-honored method, you need at least a year’s worth of hourly data. (see ftp://canuck.seos.uvic.ca/docs/MFTides/heights.pdf)
Nor is your comprehension any better about analyzing MONTHLY sea-level data,
which is a can of worms with all sorts of factors (eustatic and steric
variations, wind set-up, rainfall runoff, etc.) affecting the record even
in geologically stable locations. As your LS fitting of pure sinusoids
to the Cascais record shows, you fail to realize that it’s the presence of a
strong trend that produces your rising values as period increases. And, of
course, the well-established Rayleigh criterion for resolving sinusoids in
a record of finite length remains terra icognita for you. (It specifies
that two sinusoids can be resolved when the spectral peak of one
sinusoidal component falls on the first null of the second frequency in the
record-length dependent spectral window)
As disappointing as the Chambers et al. paper turned out to be (with it’s
simplistic bias + trend + sinusoid conception), at least they had sense
enough to remove the trend in their analysis and use the mean of
the best-fit period to the GMSL. And little is gained by removing the
annual cycle by monthly anomalization, as you do, rather than by their yearly averaging when looking for multidecadal oscillations, which no experienced geophycist would expect to be periodic.

Bart
April 30, 2014 7:27 pm

Greg says:
April 30, 2014 at 2:49 pm
See here.

April 30, 2014 9:16 pm

Steven Mosher says
Instead of cheery picking 10 stations, use them all
http://berkeleyearth.lbl.gov/regions/alaska
Henry says
FCirst, I don’t do “cheery” picking
I selected 10 stations, randomly, inland.
I was not interested in looking @sea, now, and I am not interested in results before 1998
(your Berkeley seems to report only from 1990).
If you had followed the whole thread you would know why.
but here is a good method to get a global representative sample:
http://wattsupwiththat.com/2014/04/25/the-elusive-60-year-sea-level-cycle/#comment-1622942
Clearly the Berkeley global data set lacks that balancing,as it reports a (global) warming rate of almost double that of other global data sets, including my own, from 1990.
Otherwise, why don’t you do an anlysis of all the data available from the Elmendorff Army base in Anchorage. It has data from 1942, If you analyse the maximum temperature record there and look at the average change in K/annum from 1972-2014 and from 1942-1972 you should get a part of an a-c wave that looks like the second graph shown here:
http://blogs.24.com/henryp/2012/10/02/best-sine-wave-fit-for-the-drop-in-global-maximum-temperatures/
Clearly there is still some serious cooling coming up in Alaska, Note the difference in the sine wave from Anchorage and the global a-c wave.

April 30, 2014 9:53 pm

@steven mosher
I am interested in seeing that calibration record? That must be of a new thermometer? I was talking about re-calibration.
As to error, I have deliberately chosen to look only at the average change from the average over periods of time, i.e. linear regression, in K/annum, which excludes a lot of error, especially calibration and differences between stations. Also, in older records, I trust maximum and minimum temps. more than means as the latter required presence of people and physical work, taking readings during the day.

April 30, 2014 11:33 pm

Henry.
Ur method is not BLUE. Its not proven. Its not tested.
Its wrong. Its so bad its not even wrong.
The simplest out of sample test would show you that.
Its an amateur untested flawed unreviewed piece of garbage.
Here is a simple test. Use your 10 stations to predict the 100s you ignore. Then measure your error of prediction.
It will suck. Then use the 100s you ignore to predict the ,10 you “randomly” selected. Note the improvement over
Your boneheaded approach.

Greg
May 1, 2014 12:42 am

1sky1: “As your LS fitting of pure sinusoids
to the Cascais record shows, you fail to realize that it’s the presence of a
strong trend that produces your rising values as period increases.”
The periodic analysis W used fits non harmonic patterns. It’s basically like finding the mean annual “climatology” but with varying window lengths , not just 12mo.
However, your criticism is still valid, It is the upward trend that produces what W showed and reflects his lack of experience and understanding of periodic analysis.
One of the first things to do is to remove the auto-regression and the non stationary mean, which is why the first thing I usually do with this kind of data is work with the first difference not the time-series itself.

Greg
May 1, 2014 2:03 am

Bart says:
April 30, 2014 at 7:27 pm
See here.
http://s1136.photobucket.com/user/Bartemis/media/ssn2.jpg.html?sort=3&o=22
Yes, Isn’t that something I linked you to about six months ago 🙂
I was wondering whether you had found a separate source or had reproduced it.
Oddly that links into the Stockholm temp record that our host has just published about ( comment published in Nature CS). That got me to look at SPD of Stockholm and look what I found:
http://tinypic.com/view.php?pic=lfq5g&s=8#.U2ILc6KBwrQ
I should stress that is hot off the press and unchecked, so caveat emptor.

Greg
May 1, 2014 2:11 am

Sorry is that your reworking of what the other Bart did that was produced on Talkshop?
I think you may have just explained the self convolution, that was one thing I did not get in the original. Nice one.

Greg
May 1, 2014 2:24 am

http://i1136.photobucket.com/albums/n488/Bartemis/PowerAttenuation_zpsb499835e.jpg~original
This is interesting and ties in with something else I’m doing but it’s drifting away from GMSL
Would you like to drop me a comment on my about page and I’ll get back to you?
http://climategrog.wordpress.com/about/

May 1, 2014 2:50 am

@steven mosher
why don’t you give me all your Alaska data from Berkeley from 1998, or from 2000, is also OK, if that is more readily available, and we compare that result with the -0.55K/decade I get for Alaska
(I chose 1998 because that was when earth was at its warmest)
Clearly, it is people like you standing in the way of progress,
Progress would be for you to tell the world that we are globally cooling.
.http://www.woodfortrees.org/plot/hadcrut4gl/from:1987/to:2015/plot/hadcrut4gl/from:2002/to:2015/trend/plot/hadcrut3gl/from:1987/to:2015/plot/hadcrut3gl/from:2002/to:2015/trend/plot/rss/from:1987/to:2015/plot/rss/from:2002/to:2015/trend/plot/hadsst2gl/from:1987/to:2015/plot/hadsst2gl/from:2002/to:2015/trend/plot/hadcrut4gl/from:1987/to:2002/trend/plot/hadcrut3gl/from:1987/to:2002/trend/plot/hadsst2gl/from:1987/to:2002/trend/plot/rss/from:1987/to:2002/trend

May 1, 2014 7:08 am

. Mosher
we are all waiting for you to tell us your (berkeley) result of the amount of cooling taking place in Alaska since 1998 or 2000 in K per decade
If you do not reply we will all know or notice that you are a fake and a fraud, always trying to defend AGW

Bart
May 1, 2014 9:45 am

Greg says:
May 1, 2014 at 2:11 am
There can be only one, true Bart, and that is I.

May 1, 2014 10:58 am

Willis says
Again according to Berkeley Earth, the trend 1998-present is on average -.47°C/decade, and the trend 2000-present is -1.27°C/decade.
henry says
thanks Willis. I appreciate. I am not that much interested in before. Clearly they (berkeley) are a bunch of uninformed government employees, following the masterplan, an orgaisation that has employed or engaged people like Mosher. This helps!! It proves that my estimate of cooling in Alaska of -.55K per decade since 1998 is spot on.
The acceleration to -1.27K/decade from 2000 is somewhat worrying to me. Can it be that much difference? I will check that.

May 1, 2014 11:50 am

I checked,
according to my ten sample stations , Alaska cooled by -1.05K/decade since 2000.
That worries me, as it proves my theory that we are cooling from the top, and it is accelerating as times moves on. I can see it from my global tables as well, just adding the results of 2012 and 2013. The cooling is accelerating.Exactly as predicted.
http://blogs.24.com/henryp/2012/10/02/best-sine-wave-fit-for-the-drop-in-global-maximum-temperatures/
Pity that Mr Mosher does not care.

1sky1
May 1, 2014 5:25 pm

Greg:
What W. does with the gap-filled Casais data is LS curve fitting of sinusoids of different periods, not the simple data averaging over different bin-lengths that you presume. What mislead me into thinking that the trend, which always consists of low-frequency components, was not removed was his reference to the previous chart in his write-up. Notwithstanding this mistake, which he conveniently seizes upon to call us both idiots, what he fails to grasp is the irrelevance of such curve fitting to detecting irregular multidecadal oscillations in geophysical data. And he fails to show what happens for periods longer than 80yrs.
BTW, first differencing of data is an effective mean-and-trend-suppressing stratagem, but it also severely attenuates the lowest frequencies. I’m under the gun to finish a technical report this week; I’ll have more to say when I’m finished.

May 2, 2014 1:42 pm

To Willis (and Anthony)
“Scafetta’s work has been uniformly irreproducible. Unfortunately, he doesn’t give enough information to redo his work, and he has consistently refused to show his data and code.
As a result, what Scafetta does is merely anecdote, not science in any form, and I ignore it completely.”
Anthony, when will you start to correct your guests (Willis and Mosher in primis) about this incorrect statement that my work cannot be reproducible? Holm already let you know that it can be easily reproduced with due scientific knowledge which Willis evidently does not have. Do you understand that the statement has been demonstrated to be false and constitute “defamation” under the civil code?
Said this, about the topic addressed by Willis, as usually he does not seem to understand the issue. In the case of sea level it is caused locally by different phenomena which couple climatic effects such as a changes of the volume of the glaciers, changes in the Earth rotations and changes in the ocean currents.
The phenomenon is quite complex. Let us discuss changes in water current. Water can move from one region to another. This means that in one location the sea level can rise and in another it can decrease and the phenomenon get quite complex depending where you are. Thus the 60-year oscillation is not in phase everywhere nor it is expected to be see everywhere.
In some record it is quite evident in other it is less evident.
As Mosher noted above in my paper
Scafetta is another author showing an ~ 60 year cycle in long sea level data.
Discussion on common errors in analyzing sea level accelerations, solar trends and global warming Pattern Recognition in Physics 1, 37-58.
http://www.pattern-recogn-phys.net/1/37/2013/prp-1-37-2013.pdf
I analyze the record from New York and this long record (since 1860) show it quite clearly.
See my figure 3.
However, Mosher did not noticed that In my paper I have not analyzed only the record from NY but in Figure 2 I have analyzed the global sea level reconstruction by
Jevrejeva, S., Moore, J. C., Grinsted, A., andWoodworth, P. L.: Recent global sea level acceleration started over 200 years ago?, Geophys. Res. Lett., 35, L08715, doi:10.1029/2008GL033611, 2008.
ftp://soest.hawaii.edu/coastal/Climate%20Articles/Jevrejeva_2008%20Sea%20level%20acceleration%20200yrs%20ago.pdf
This global reconstruction of sea level does show a quasi 60 year oscillation. since 1700.
Note that in their paper Jevrejeva et al wrote:
“Superimposed on the long-term acceleration are quasiperiodic fluctuations with a period of about 60 years. ”
The issue, now, is to see whether the patter is an artifacts of the data. To show this one needs to compare with other records since 1700.
This was done in
Scafetta N., 2013. Multi-scale dynamical analysis (MSDA) of sea level records versus PDO, AMO, and NAO indexes. Climate Dynamics. in press.
http://people.duke.edu/~ns2002/pdf/10.1007_s00382-013-1771-3.pdf
See figure 10 where the there is comparison with the NAO index since 1700, and this index shows the same quasi 60-year oscillation.
This is enough to respond to Willis both about the merit of the 60-year oscillation in the SL and the reproducibility of my work.

Greg
May 4, 2014 2:55 am

1sky1: “BTW, first differencing of data is an effective mean-and-trend-suppressing stratagem, but it also severely attenuates the lowest frequencies. I’m under the gun to finish a technical report this week; I’ll have more to say when I’m finished.”
Which is exactly what red-noise, random walks and auto-regression is all about.
It is the auto-regression that creates a lot of the long term variability. That does not make the variability less real but working with first diff puts any random noise back into a “white noise” spectrum.

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