ea
th
,
th
e
m
et
ho
d
u
se
d
at
th
is
st
ag
e
fo
r
th
es
e
st
ak
eh
o
ld
er
typ
es
is
sp
ec
ied
.Sh
oul
d
ther
e
be
tw
o
o
r
mor
e
model
sbein
g
develope
d
in
th
e
process
,the
n
th
e
typ
e
o
fmode
lt
o
whic
h
th
e
metho
d
wa
s
applie
d
is
show
n
in
parentheses
.O
T
re
fe
rs
to
th
e
co
m
po
si
tio
n
o
ft
he
o
rg
an
iz
in
g
te
am
.
Fo
r
o
rg
an
iz
in
g
te
am
in
vo
lve
m
en
t
in
di
ffe
re
n
t
pa
rt
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
reanalysis project is 37h1.2. The simulations were run on the c2a supercomputer
at the European Centre for Medium Range Weather Forecasts (ECMWF). The model domain is
the same as the one used for the IMO operational forecast runs (DOMAIN=ICELAND)2, with
300 240 horizontal grid points, and a horizontal grid-point spacing of about 2.5 km in both
directions.
HARMONIE uses a terrain-following sigma
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
Meteorological Office (IMO) between 2011 and 2014. The model do-
main is also the same as for the IMO operational runs, with 300 240 horizontal grid points cov-
ering the whole of Iceland and parts of the surrounding ocean, and with a horizontal grid-point
spacing of about 2.5 km in both directions. The model is run with the standard 65 vertical levels,
and with a non-hydrostatic dynamic core
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
A suite of possible mechanisms
are calculated for each event based on polarities and spectral amplitudes. Through the joint
interpretation of fault mechanisms with the event distribution defining the fault, the slip
direction on the fault plane can be inferred. Using this kind of mapping, about 240 faults,
fault segments and small clusters, which were active in year 2000, have been mapped
during
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf