Sunday, 2 December 2012
First Advent
Sunday, 25 November 2012
Back on track in Utsteinen
Monday, 19 November 2012
The Antarctic summer season has started
Friday, 6 April 2012
Being back and staying connected



It’s now already six weeks ago that I left Antarctica and that I am back in Belgium. Normal working life takes over rapidly. It has been time for debriefing meetings, for securing the data and to proceed to first preliminary data analysis, but also to think already what tasks have to be done during next season and what this means with respect to sending staff and cargo.
From the Belatmos instruments, three of them are still operational – the aethalometer, the TEOM-FDMS, and the laser aerosol spectrometer. The aethalometer and TEOM-FDMS are storing the data on their internal data storages and will be read out next season. Concerning the aerosol spectrometer – it is connected via an Ethernet cable to the internet. Therefore, I can regularly check the size distribution data and also download the current data. This also means that at this moment, the power supply of Princess Elisabeth station is still working. Let’s keep fingers crossed.
Above, I put some preliminary plots with examples of aerosol data. The top image shows the total scattering coefficient measured by the nephelometer at 635 nm for roughly two days (of 5min average data). These coefficients are given in units of Mm-1 (or 1*10-6 m). The scattering coefficient correlates well with the overall amount of ambient particles – the more particles there are, the higher the scattering coefficient. However, at the same time, aerosols do scatter and absorb, and the more scattering compared to absorbing they are, the higher the scattering coefficient will be. Values like shown in the graph represent low overall aerosol concentrations.
In the middle graph, the total number concentration detected by the condensation particle counter (CPC) is shown for two hours (1min averages) from the same period. The overall particle concentration was around 600 to 700 particles per cm-3. The few much higher peaks indicate very probably the measurement of the exhaust of skidoos or prinoths passing by nearby. However, this has to be analysed and confirmed in more detail. As mentioned in a former post, the usual concentration in sub-urban regions would be 10 to 100 times higher.
The bottom image gives the number size distribution over the two hours of the total number concentration of the middle graph. Although the laser aerosol spectrometer can only measure from a particle size of 90 nm onwards, the dominant size around 100 nm was within the measurement range. It also can be seen that there are hardly any particles larger than 1 micrometer. In a further analysis, I will combine the two measurements of total number concentration and of size distribution to define the concentration within the range 3 to 90 nm – as the CPC is measuring all particles from 3 nm onwards.
Tuesday, 21 February 2012
Last Days
Today is the last day for me at Princess Elisabeth station. Tomorrow we will fly to the Russian Novo Air Base and on Thursday then to Cape Town. The last days are filled with de-installing the instruments which have to go back to Belgium for calibration or adaption reasons, and to prepare the other instruments for winter operation. All my instruments have been measuring fine so far, so I am right away satisfied. There was a lot of sunny weather, and the ozone spectrophotometer and the sun photometer had done a lot of good measurements. Also the condensation particle counter (measuring the number of particles in the air) turned out to behave smoothly. Most of the time there are low particle concentrations of around 300 to 500 particles per cubic centimetres. If one would measure, e.g., in Brussels, the concentrations were 100 to 1000 times higher. Our instrument is really sensitive – detecting immediately if the station’s bulldozer, tractor or somebody smoking is passing nearby. The last days we take advantage of the calm weather for clearing the garage’s roof from the huge amount of snow/ice which has accumulated over the last winter. We were moving tons of snow/ice. One block of around 50x50x50 cm of this compacted snow weighs approximately 70 to 80 kg. On Sunday I also went with Denis from the Observatory to dig a 1 m snow profile in order to better understand the snow accumulation over the winter. These measurements are needed for the ‘Hydrant’ project of the KU Leuven, from whom nobody could come this season. At such a profile one measures the temperature profile, determines how many layers are distinguishable, and within these layers one describes the ice crystals size, form and the hardness of the snow. In addition, from the layers snow samples are taken in a normed cylinder and this is weighed. This weight is then converted in water equivalent and is then used to estimate the amount of precipitation over the accumulation period. On the images, the Utsteinen nunatak and the station on the small Utsteinen ridge can be seen. On Monday, we got a bit more wind and this was announced earlier by the forms the clouds form over the Romnoesfjellet peak towards north, around 60 km from Princess Elisabeth station.
