and the Eastern Volcanic Zones (WVZ and EVZ (Figure 1). The two
segments are connected through a 70–80 km long transform zone, the South Iceland
Seismic Zone (SISZ), which regularly produces a sequence of large, destructive
earthquakes of magnitudes up to M7 (Einarsson et al., 1981; Einarsson, 2008). The
majority of the rifting is taken up by the southward propagating and much more active
EVZ
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
morning, around 2.600 earthquakes have been detected with the earthquake monitoring network of the Icelandic Meteorological Office (IMO). Throughout the whole sequence the majority of events has been at 5-10km depth. No signs of migration towards the surface or any other signs of imminent or ongoing volcanic activity have been detected. IMO is monitoring the area closely and will update in case
/earthquakes-and-volcanism/articles/nr/3000/
the stochastic residuals are added as random numbers (the last
panel). The tendency of the realizations of temperature and precipitation change to fall on
straight lines in Fig. 3.6c is artificial – this is due to the fact that the same sequence of random
numbers is used for both variables. As implemented here, the method does not take into
account the correlation of temperature and precipitation change
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf