Understanding earthquake figures.
or [Cherry] Picking Your Data - An introduction to earthquake charts.
This is in reply to post by muzzy
I have had time to take a look at the Kuril Islands properly now. Just doing the
radius view from the epicentre of the last quake gives the wrong
impression in some ways.
First let us take a look at all earthquakes Mag 5+ from 1900 using the
Centennial
catalogue and
ANSS to bring it to the start of 2012.
I have to say that I have not looked in depth into the sources of the centennial but I suspect that much come from the NEIC and ANSS.
The data is sparse in the earlier years as no Mag 5+ quakes were recorded. It important to understand the population of the catalogue at this
point.
For recent years (1964 - present) a cut-off magnitude of 5.5 has been chosen for the catalog, and the catalog is complete down to that threshold.
For the period prior to 1964 (also referred to as "historical instrumental" or simply "historical" period) the cut-off considered is magnitude 6.5.
Between the 1930's and 1963 the catalog is complete to the magnitude 6.5 threshold, but prior to that, the catalog is only complete down to magnitude
7.0.
Next I looked at 1963 to present. The reason I took 1963 was to include the 8+ in 1963 which would not have been there if I used 1964. Mag 5 stated is
of course mag 5.5 until 2002 when the ANSS data kicks in.
There is an interesting 'gap' between 1997 and 1999 for which I have no explanation. You can see the effect of the ANSS catalogue kicking in.
Now so far the 'trend' on these two has been up. By picking the first graph and not explaining the catalogue it would be possible to give the
impression that earthquakes were seriously on the increase. Selecting data from around 1973 is common, not always as an exercise in cherry picking but
purely because the ANSS/NEIC catalogues pretty much start at that point in earnest.
During this time (from 1970 onwards) of course coverage of areas by instruments increased. There were about 350 stations globally in 1930 and around
2000 by the start of the 1970s. With the arrival of the digital seismograph this took off and now there are in excess of 8000 instruments worldwide
that contribute to the global networks and catalogues.
So the figures for Kuril from year 2000, with the benefit of all that technology, look like this.
Now the trend has gone down. All three of these graphs have been unaltered except to shorten the dataset. The trendline computation is the same for
all three.
The USGS
has a set of graphs showing the number of earthquakes in each
decade going back to 1980.
Here is a statement from a very widely quoted blog with a graph that keeps on turning up time and time again as 'proof' that earthquake numbers are
increasing.
Below is a graph showing how the number of all magnitude earthquakes has grown over recent years.
Source
Graph above provided by DL Research. -
www.dlindquist.com...
The author of the graph states on his site that:
It provides a comprehensive picture of US Geological Survey data from the 1970s until today, and exposes some interesting trends in seismic
activity
In fact what it exposes is the lack of knowledge and diligence in research by the author in what he designates his 'Research' section. No mention of
the number of stations is made, or of other factors. His graph so widely promulgated stops in 2006. You can see a downturn at the top. So, does anyone
ever go back and look at the current situation? No. The reason is this.
The chart from the same site for all magnitudes running up to 2012 shows a
marked downturn. No web doom-sayer would want to quote that!
Question is what has happened here?
It is actually very simple and illustrates what I have said time and time again that numbers do not matter, energy does. USGS, upon which his data is
based, made a decision to retain only earthquakes of Magnitude 4.5, or 4.0 if reported as felt.
This graph shows the 'World' figures as a stacked column so you can see the components. This is only 1990 to 2012
Now, if I remove the quakes under Mag 5 the chart looks like this.
The chart of the totals shows what a dramatic difference removing the earthquakes under mag 5 (effectively) has on the chart. Where the 'world' figure
drops dramatically in 2009, the US figure goes up.
So upon what data can one depend? It has effectively been stated - back to 1964 you can count on 5.5 BUT a word of warning here. We, the quake nerds,
know for a fact that even today there are magnitude 5.5+ earthquakes (depending on the scale) that do not get picked up so be aware. Back to 1930 you
can depend on 6.5, again however I personally would be a little wary for the data before around 1950 and suggest it may not be as complete as they
would like to think. From 1900 you can depend on 7.0, and here I would agree that aside from the magnitude scales problem, which I will cover in the
next quake nerds corner, this is probably OK to use. But what use is just looking at mag 7 earthquakes you ask?
I have recently taken to producing what I call "stress sawtooth graphs" which attempt to show the possible energy that is accumulating in an area.
Obviously these will be affected by the number of mag 5 and 6 earthquakes - or will they?
Here is a stress tooth using exactly the same data as for the first graphs above - the Kuril Islands. The first is earthquakes of Mag 5.5 upwards, the
second is Mag 6.5 upwards and the third Mag 7 upwards. Bear in mind that there are 5.6 Mag 6.5 quakes in a Mag 7.0. The columns are the same on all
three graphs.
No, they are not all the same, but the difference is so small that it is almost imperceptible. I can happily use the mag 7 values back to 1900 and
know that it makes no difference to the stress calculation overall.
I can't load it here are it is too big but here is a small version of all three as a gif so you can see the changes
Magnitudes and Energy in the next Quake Nerds Corner on April Fools day.
For more details on Mag 7 earthquakes world wide visit:
MAJOR WORLD EARTHQUAKES ~ mapped, graphed and listed ~ 314-2012
edit on 29/2/2012 by PuterMan because: (no reason given)