(F ð1; 905Þ ¼ 6:89,
po0:01, partial Z2 ¼ 0:008), and a larger reduction in own and others’ car
use compared to the increase with two SEK/l (F ð1; 880Þ ¼ 16:96, po0:001,
partial Z2 ¼ 0:019 and F ð1; 879Þ ¼ 15:64, po0:001, partial Z2 ¼ 0:017
respectively). In addition, the increase with five SEK/liter was perceived as
more unfair (F ð1; 904Þ ¼ 10:06, po0:01, partial Z2 ¼ 0:011) and respon-
dents
/media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
possible. There is a constant stream of real-time seismic
data coming into the monitoring office from over 80 seismometers located around the country,
allowing the IMO to monitor over 30 active volcanic systems in Iceland as well as two major
seismic fault zones. With the presence of so many active volcanic threats, effective monitoring
and warning systems are essential.
Plots of Real-time Seismic
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
236
1992 09 167 124 167 98
1995 07 1994 1759 599 368
1995 10 96 62 73 37
1997 07 921 728 330 184
2000 08 1240 1083 365 221
2002 09 689 582 267 160
2003 11 241 207 139 98
2006 04 1370 1340 300 270
2008 10 1350 1290 300 265
The origin of the 1957, 1960, 1964 and 1966 jökulhlaups is not certain but is most likely the eastern cauldron. The discharge
and volume for the 1995 jökulhlaup are a sum from
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf