0.95
vhm149 1.46
vhm205 1.01
vhm206 1.28
vhm221 0.9
vhm265 1.16
vhm277 0.87
vhm278 -0.12
18
l
l l l
l
llll
l
llll
lll
ll
lll
lllll
lllll
ll l
l l
l
l
l l
l l
l
l
−2 0 2 4 6
0
1
2
3
4
−ln(−ln(1−1/T))
Q/
E[
Q]
1 2 5 10 20 50 100
T (years)
l
l
l
l
l
l
l
l
vhm148
vhm149
vhm205
vhm206
vhm221
vhm265
vhm277
vhm278
Regional +/− 95% CI
H1 0.995
H2 −0.877
l
l
l
l
l
l l l l
l
l
l l
l
l
l
l
l
l
l
l
l
l
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
Ito, K. (1990). Regional variations of the cutoff depth of seismicity in the crust and their
relation to heat flow and large inland-earthquakes, J. Phys. Earth., 38, 223–250.
Jakobsdóttir, S. S., G. B. Guðmundsson and R. S. Stefánsson (2002). Seismicity in Iceland
1991–2000 monitored by the SIL seismic system. Jökull, 51, 87–94.
Jakobsdóttir, S. S., M. J. Roberts, G. B. Guðmundsson, H
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
14 0 1 2 3 8 12
15 0 1 2 3 8 12
16 0 1 2 4 8 12
17 0 1 2 4 8 12
18 0 1 2 4 8 12
19 0 1 2 4 8 13
20 0 1 2 4 8 13
21 0 2 3 5 9 13
22 1 2 3 5 9 13
23 1 2 3 4 9 13
MEAN 1 2 2 4 8 13
10
AE
R
OD
R
OM
E
CLIM
A
T
OLOGICA
L
SUMMA
R
Y
-
T
ABL
E
D
AE
R
OD
R
OME
:BIK
F
-
KEFL
A
VÍ
K
/K
efl
avi
k
PERIO
D
O
F
RECORD
:2001–201
0
L
A
TITUDE
:6
3
59’06"
N
LONGITUDE
:2
2
36’20"
W
ELE
V
A
TIO
N
AB
O
V
E
MSL
:5
2
/media/vedur/aerodrome_summaries_20140603.pdf
for Iceland were made. The CE
project used an ensemble of six GCMs and RCMs from the PRUDENCE project for four different
emissions scenarios (B1, B2, A2, and A1FI) developed by the Intergovernmental Panel on Climate
Change (IPCC). The GCMs used by the CE project showed more warming during winter than
summer. During winter, the median projected warming from 1961–90 to 2070–99 ranged from
3–6 K, and from 2
/media/ces/2010_005_.pdf