Thursday, 31 July 2014

Trends 2014 - completed

Trends 2014 meeting was successfully completed. A number of topics were covered. For me personally, the most interesting new information was that the trends affect the space debris population. Hence, we need to follow the foF2 and hmF2 trends... and of course EISCAT and EISCAT_3D space debris measurements are important in this business! Also, bit of Ethiopia news: American colleagues will install two Fabry-Perot interferometers to Ethiopia during the coming autumn!

I presented my own stuff today and talked about dynamic linear models and estimation of time-varying hmF2 trend of the Sodankylä ionosonde data (see Figure below).

Hence, time to travel up to Sodankylä, ETA Friday evening 23 LT! (stopping at London for Th-Fr night)
hmF2 dynamic trend for Sodankylä 1957-2014.

... and presenting my stuff! (photo: Erkki Kyrölä, FMI)

Monday, 28 July 2014

Trends 2014, Cambridge UK, July 28-31

This week, in Cambridge UK, takes place 8th Workshop on Long-Term Changes and Trends in the Atmosphere 2014. The meeting started on Monday morning and will run until Thursday afternoon. I will have my talk on Thursday! As this meeting is not 'inverse problems', i.e. I am out of my comfort zone, so today we will simply feature photos from the conference venue Clare College. (It is absolutely stunning and beautiful college.) I will come back to the science covered later this week (hopefully) !!









Sunday, 27 July 2014

Hengenvaara

Last week we went for a bit of a walk to the FMI radar at Luosto. On the way, we passed some little hut... probably an electric power distribution box.


On the door was a sign... "Hengenvaara"


Now, if I understand this correctly:  "vaara" is "hill"... as in Pittiövaara or Lampivaara.

Of course this is not to be confused with "väärä", which would be "incorrect" (and also incorrect).

And "hengen" (as in "henki") is "spirits" or "souls"... or something.

So, does that mean that this hill is haunted? And, if so, by whom?

Well... probably the person who mistranslated the sign and was subsequently electrocuted!

Friday, 25 July 2014

Meet the press

We had a visit from a reporter this week, to interview some of the staff about KAIRA, the Centre of Excellence for Inverse Problems, EISCAT and the general operations of Sodankylä Geophysical Observatory. So, reporting on the reporting, today we have a photograph of just that!

Lassi and Esa being photographed in front of the 32m dish.

Have a nice weekend everyone!

Thursday, 24 July 2014

Ionospheric "Scintillation Arcs"

Compact radio sources twinkle (“scintillate”) because of variations in density moving around in the interstellar medium, the solar wind and the Earth's ionosphere, in exactly the same way as the visible stars scintillate due to the Earth's atmosphere. This scintillation has been studied for many years and is used as a way of probing these density variations and gleaning information about, for example, the density and velocity of the solar wind.  With KAIRA we have been observing ionospheric scintillation since operations started in 2012.

When viewed as a time series, the scintillation manifests itself as rapid variations in received intensity. If the received signal is also split up into a number of frequency channels across the available bandwidth, the time series' for each channel can be stacked and plotted in a dynamic spectrum which shows how the pattern of scintillation varies with both observing frequency and time.

In modelling the scintillation, we often assume that the signal is scattered by a “thin screen” of density variations (imagine an irregular grid through which light might be diffracted), moving at a certain velocity relative to the radio source. The scattered waves then interfere as they travel further from the screen and the resulting interference pattern is what we receive as scintillation. Multiple thin screens along the line sight can be used to model scattering due to a thicker medium.

Now imagine pairs of waves being scattered by the thin screen: Each pair of scattered waves has a Doppler shift due to the movement of the screen and a time delay between them due to the different path length that each wave has likely followed. A “map” of these Doppler shifts and time delays between every pair of scattered waves can be formed by taking the so-called “secondary spectrum” - effectively the 2-dimensional power spectrum (squared amplitude of the 2-dimensional FFT) of the dynamic spectrum. When this analysis is applied to pulsar observations to study scintillation in the interstellar medium, a clear arc structure termed a “scintillation arc” (first discovered by Dan Stinebring in 2001), is often seen. Over the years this has proved an invaluable tool for probing the interstellar medium.


Now, for we believe the first time, scintillation arcs have been found in the secondary spectra of ionospheric scintillation seen in observations of Cygnus A taken using the KAIRA. It is believed that these also represent the first such broadband (relative to the observing frequency) observations of arcs due to any scattering medium and also the first found using LOFAR hardware. These results have now been written up in a paper recently submitted.

The image shows an example segment of dynamic spectrum and an example secondary spectrum, with the x-axis being Doppler shift and the y-axis being a parameter equivalent to time delay.

Wednesday, 23 July 2014

Weather radar

Yesterday we described our walk up the ski slopes of Luosto on that hot summer's evening. But what was at the top?

Well, it turns out there is a large weather radar (= säätutka) there. This is operated by our colleagues at the Finnish Meteorological Institute (FMI).

The "blue stone". (Photo: D. McKay-Bukowski)

The FMI weather radar site. (Photo: D. McKay-Bukowski)

Lassi ignores the warning signs. (Photo: D. McKay-Bukowski)

It's a really lovely place. A bit like a lighthouse. A pity it is remotely operated, as I'd so love to work in a place like that.

Tuesday, 22 July 2014

A bit of a walk

Along similar lines to the recent post on swimming, we have another little adventure. This was the decision on Monday evening to go for a walk... this time to Luosto. Lassi organised this, similar to our excursion last year to Viiankijärvi, which was a chance to get outdoors away from the work and see some Lappish scenery.

Anyway, there are some ski slopes there not far from the Amethyst Mine, and we climbed up the hill there. Today, we have a couple of photographs from that trip... in stark comparison to the conditions of last January. Remember our scene from last time?

Intrepid adventurers from SGO. (Photo: D. McKay-Bukowski)

The ski-slopes... looking forlorn in the summer. (Photo: D. McKay-Bukowski)


Still a great walk, with lovely weather conditions. (Photo: D. McKay-Bukowski)

After the discovery of the giant river pike after our bit of a swim, we might have been quite nervous about what we might have found at the top of the mountain. And indeed there was something quite unusual at the top.

But you will have to wait until tomorrow to find out what it was!