Arctic sea ice June 2011
Since I’ve not shown anything to do with sea ice recently, here is an update on Arctic sea ice extent.
Daily data from IJIS/JAXA.
I’ve modelled the annual cycle and subtracted from the data.
There is still no obvious change making it clear where the Arctic ice is going to meander next.
Data
Is sea level really an issue?
- Normalised sea level and temperature
This is likely to be controversial and dismissed by some as invalid, which is their problem.
The RSS data is monthly.
Topex/Jason data is sampled roughly every 10 days, processed into monthly and then normalised to the RSS data.
Both month data were low pass filtered at 10 years, with end correction. This is likely to be dismissed as impossible, look, it is self evidently about right.
All four are plotted above.
Other work has suggested there is a correlation between temperature and sea level, sea level lagging perhaps 4 years. (I doubt many people think that sea level causes temperature)
The actual sea level rises being talked about are extremely small relative to the size of the planet.
What if the top few x metres of sea water are warmed by 0.2K?
What if the Vostok core is like polar ice?
With the last post I hope I demonstrated how a very simple regular function, a planet orbit, causes a more complex modulation of sea ice, something which does not seem to be generally understood.
Look back a couple of posts and you will see Vostok ice core plots.
What I have done now is flip the temperature proxy data upside down. This ought to roughly represent ice and puts the data the same way around as the earth sea ice plots. More ice is upward, melt is downwards.
I then used a very crude approximation to some kind of orbital signal, actually locks in at 103ky.
This is known wrong in relation to orbits (explain more in a moment) but food for thought.
Do you now see why the widespread notion that sharp melts cannot come from a simple stimulation is a highly questionable assumption? It should be considered feasible and with no magic or particular non-linearity.
Assistance
I would appreciate assistance with very long orbital period calculation. I have the capability to carry out some novel experimentation using accurate orbital data, which I do not have.
One of the very interesting features is apparently the variation in the eccentricity of the earth orbit on these very long timescales, ie. it varies with at least two periods. I hope the reason why this is so interesting is not lost on the reader.
How polar ice is modulated by the sun
What follows here is a demonstration of how earth orbit shapes Arctic ice and in a later post I intend to show how this may well relate to palaeoclimatology shown in ice cores.
You will have seen the plots of Arctic sea ice. I am going to use one dataset here, which one is unimportant, others give the same answer.
Epica Vostok resampled composite
I won’t say much here now, busy.
This seems to confirm a huge date mistmatch between the two sets of ice core data.
This is a deliberately large plot. Contact me if you need data or help.
Simplest way to provide data is an export to XLS format of work, warts and all.
Contains usable resampled data and originals
Added later, easiest way to provide data is export to XLS, is scruffy workfile
Vostok ice core, part 2
See part 1 if you haven’t.
Seemed a good test to see if I could reproduce the temperature vs. CO2 lead lag result but using signal processing, data resampling. Turns out the CO2 data is even worse than the isotope ratio temperature data, fewer data points and sampled at different dates.
Easy. I applied identical processing to both datasets and then figured out how to time shift one of them. To my surprise there is a very high correlation, r2=0.82, at least given the preprocessing used. The quick and dirty way to do the time shift was apply an offset at the decimate stage, simply picks off data at a different point. (this is valid)
If I have done this right it is about 1,500 years for best fit of rise and fall. I then aligned the datasets and plotted (Y axis reacaled and offset CO2 by hand so the data roughly matches on one scale) for an eyeball.
There is obviously a lot going on but there it is visibly on one plot.
A net dig shows a work by Jo Nova (know the name, no idea who she is)
http://joannenova.com.au/global-warming/ice-core-graph/
That says 800 years and seems to cite others.
Ref
http://www.ncdc.noaa.gov/paleo/metadata/noaa-icecore-2453.html
ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/vostok/co2nat.txt
Vostok ice core, part 1
Length of Day, modelling the lunar and annual effect
As a result of helping someone out with lunar effects in Earth length of day I wondered if a slightly more comprehensive version would work.
The result is an interactive spreadsheet which might be useful.
I would not usually produce such a monster, this is an xls >30Mbyte but it does include reconstruction of the lunar LoD signal, subtraction from the raw LoD and decimation for plotting. It is live, you can turn on or off individual terms/factors and see the effect.
This needs a great deal of explanation, codas, and so on.
For now here is the file lod-work
Do not try this unless you have a fairly large computer. Checked it works with gnumeric, openoffice/libreoffice. Excel should not have a problem but recursion is used.
Circles and dimensions
Gold appeared during a detailed technical web search, complete wrong context for what I wanted but one of the strangest happened upons ever for me.
I will present the cross check first, this has a very real basis.
The Wiltshire Heritage Museum is based in Devizes, Wiltshire. Not so far from here and now I must visit when the opportunity arises. I know the henge area, where my father grew up, know this from the times where our heritage was ours and not stolen by the exploiters.
http://www.wiltshireheritage.org.uk/
A bizarre artefact held Is the Bush Barrow “lozenge”
http://www.wiltshireheritage.org.uk/galleries/index.php?Action=3&obID=89&prevID=9
A new zealander has written his interpretation of what this is
http://www.celticnz.co.nz/BBLOZ/BBLOZWEB1.htm
Enjoy.
Out of politeness here is his home page where there is a lot more in articles
http://www.celticnz.co.nz/
ERBS TSI
As part of an ongoing investigation I looked at the ERBS TSI data. This dataset is not particularly interesting and as with all satellite data is far too short to say much. One interesting snippet did appear.
Creating a rough model posed some problems but in practice was simple.
First was the data has a Y2K corrupted date which was kindly sorted out by V.
The sampling is irregular (scattered time points) which the software can usually handle if slowly. The result is unremarkable.
I’ve shown a fore and hindcast which indicates the model is stable and sane. It will be somewhat wrong.
A surprise came when I looked at a paper associated with the dataset where the final sentence of the conclusion is “The fact that the measurements increased with time relative to the proxies suggests the existence of a second TSI variability component with an amplitude greater than 0.04% (0.5 Wm-2), and with a period greater or equal to approximately 20 years.”
A minor model component: 20.0432969909 3.69480925972 0.124480125667
Period just over 20 years, amplitude 0.125 * 2 * sqrt(2) = 0.35W p-p
With such short data that will be way out and TSI certainly is far more complex in the long term.
http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.81.834&rep=rep1&type=pdf
I’ve shown SORCE as well. This is not really TSI, is narrowband/is in my opinion incomplete [disputed, see comments]. It does however show the wide variation is measured values. Given the extreme difficulty in making these measurements the usual rule of thumb is sensible, the instrument must be at least an order more accurate and so for absolute maybe we know +-40W sq/m
Putting that into context 40W in 1360W is +-3% of absolute, not as easy as many will imagine and for a remote instrument is an intensely hostile environment would not be a surprise. Lets hope the instrument is returned to earth for post mission calibration checks. See the point?
“Validation of spacecraft active cavity radiometer total solar irradiance [TSI] long-term measurement trends using proxy TSI least squares analyses
“aRobert Benjamin Lee III and bRobert S. Wilson
aNASA Langley Research Center, Atmospheric Sciences, MS 420, Hampton, VA 23681-2199
Science Application International Corp. (SAIC), One Enterprise Parkway, Hampton, VA 23666 “
http://www.acrim.com/
A lot of interesting material on TSI can be found here http://www.leif.org/research/









