will be compared to possible problems to
see if this is actually a problem. The completeness of the data series is discussed in section
6.
Table 7. Power connection.
Type of communication Number of stations
Main Power 35 (55%)
Produced on site 28 (45%)
For CGPS stations reliant on remote power sources, the preferred solution is a photovoltaic
solar panel and a wind generator. However, several
/media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
in Iceland: Climate projections and historical changes in precipitation type Andréa-Giorgio R. Massad, Guðrún Nína Petersen, Halldór Björnsson, Matthew J. Roberts & Tinna Þórarinsdóttir99
20,6
/about-imo/publications/2022/
Kjøllmoenet al. 2007).Storbreen is located just east of the main waterdivide between east and west in southern Norwayand receives precipitation from both directions(Liestøl 1967). The glacier is part of an east–west
mass balance transect in southern Norway where
mass turnover is largest near the western coast anddecreases towards the drier interior (Andreassen etal. 2005). Storbreen is in this respect
/media/ces/GA_2009_91A_4_Andreassen.pdf
Amplitude Measurement (RSAM) data are one of the most
important tools utilized in volcano observatories worldwide. The IMO’s monitoring office is
no exception, as this type of real-time data shows mid- to long-term trends, which is especially
important for monitoring active volcanic systems. The RSAM methodology was developed by
the USGS in 1989 (Murray & Endo, 1989) to plot averaged amplitude
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
................................................................................................................. 45
6 DISCUSSION ...................................................................................................................... 49
6.1 Differences in return levels between observed and simulated precipitation ..................... 49
6.2 Sensitivity of the EVA methods
/media/vedurstofan-utgafa-2020/VI_2020_008.pdf
). Photo taken at 17:45.
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K. Maack, Director General Icelandic CAA
Ash measurements, experience 2010 and 2011
9:45 Eruptions in Eyjafjallajökull, Etna and Grímsvötn, airborne OPC measurements and quality
assurance Konradin Weber, UAS, Düsseldorf Germany
10:15 Observations in plumes and vicinity of airports Jonas Eliasson HÍ (UI)
Initial and boundary data acquisition and improvements in modelling
10:45/media/vedurstofan/utgafa/hlidarefni/program17012012.pdf