are used, the estimated quantiles are
relatively unbiased in average and are usually within the 95% CI of the reference quantiles in
a majority of target sites. Poor quantile estimates are obtained for catchments where bµi(D = 0)
is most biased. The corresponding RMSET varies between 28% of the reference quantiles with
IFM-WaSiM to 39% with IFM-CLU (Fig. 13).
28
l
l
l
l
l
l
l
l
l
l
l
l
2 4 6 8 10 12
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
have been located in Bárðarbunga and 15 in the intrusive dike.
The largest earthquake since midnight was M 5.5, located at the southeastern caldera rim. This earthquake is among the largest measured at this central volcano since the onset of these events, 16 August. Up til now, four other quakes have been about 5.5 and one more definately larger, M5.6. All in all, 39 earthquakes have been M 5.0
/earthquakes-and-volcanism/articles/nr/3001/
.......................................................................................................... 38
Figure 17: Probability of location of future vent opening based on the locations of identified
previous vents using a Gaussian kernel-smoothed function model ......................................... 39
Figure 18: Monthly foreign visitors to Heimaey in 2016 ........................................................ 42
Figure 19: The probability that tephra released
/media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
estimates for large earthquakes in SW-
Iceland. Icelandic meteorological Office Report (in preparation).
Wurman, G., Allen, R. M. & Lombard, P. (2007). Toward earthquake early warning in
northern California. J. Geophys. Res., 112, B08311, doi:10.1029/2006JB004830.
37
3. Intensity vs. peak ground acceleration (PGA) and
peak ground velocity (PGV) in SW-Iceland
38
39/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf