the two reanalyses exist primarily over Green-
land, where the amplitude of the seasonal cycle in ERA-Interim is reduced, with up to 5 K higher
temperatures than ERA-40 in winter, and up to 5 K lower temperatures in summer (not shown).
Elsewhere, differences are small and unsystematic.
As described by Simmons et al. (2006) and Berrisford et al. (2009), compared with ERA-40, sev-
eral improvements
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
and providing early-warning mechanism information.
Figure 1. Map showing SW-Iceland, the focus area within SAFER. Seismicity during
1997–2000, defining many of the already mapped faults, is shown colour coded
according to age. Events with M>5 are shown as stars. The outline of the South Iceland
Seismic Zone (SISZ) is shown with orange dashed lines. Test sites are marked on the map
with letters K, H, Á
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
version of the manuscript.
References
Allen, R. M., G. Nolet, W. J. Morgan, K. Vogfjörd, M. Nettles, G. Ekström, B. H.
Bergsson, P. Erlendsson, G. Goulger, S. Jakobsdottir, B. Julian, M. Pritchard, S.
Ragnarsson, and R. Stefansson (2002). Plume driven plumbing and crustal formation in
Iceland, J. Geophys. Res., 107 (B8) 101029/2001JB000584.
Ágústsson, K., and Ó. G. Flóvenz (2005). The Thickness
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
su
lta
tio
n
o
f
st
ak
eh
ol
de
rs,
co
m
m
en
tin
g
an
d
o
bje
cti
ng
o
n
go
al
s
an
d
tra
ns
bo
un
da
ry
as
pe
ct
s
(Ens
erin
k
et
al
.200
3;
Raa
dgeve
ran
d
Mos
ter
t200
5).
Asse
ssmen
to
fexi
stin
g
situatio
n
D
at
a
(na
tu
ra
ls
ys
te
m
s):
1:
Ep
ist
em
ic
O
fte
n
do
m
in
an
t
In
te
rn
at
io
na
lm
o
n
ito
rin
g
n
et
w
or
k
se
tu
p,
i.e
.thr
oug
h
IC
PR
.Su
stainabl
e
tra
ns
bo
un
da
ry
co
o
pe
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
variability pattern on a decadal scale,
mainly through wind and pressure forcing but also through steric effects (Dangendorf, Calafat, et
al., 2014; Dangendorf, Wahl, et al., 2012; Madsen, 2009; K. Richter, Nilsen, and Drange, 2012;
Yan, Tsimplis, and Woolf, 2004). Decadal sea level variability over open North Atlantic ocean,
especially the Subpolar North Atlantic, in the satellite altimetry era
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
.................................................................................................................................................. 24
Tietäväinen, H., Ylhäisi, J. and Jylhä, K.
Summertime Precipitation in Finland under Recent and Projected Climate ......................................................... 26
Pryor, S.C., Barthelmie, R.J., Schoof, J.T., Clausen, N.E., Kjellström, E. and Drews, M.
Intense and extreme wind
/media/ces/ces-oslo2010_proceedings.pdf
of the page
Í
ÍsafjörðurWest fjsjObs.ForecastMeteogramInfo.Obs. data
Return to the top of the page
J
JökuldalurE coastalsjObs.Info.Obs. data
JökulheimarCentralsjObs.ForecastMeteogramInfo.Obs. data
Return to the top of the page
K
KaldakinnNorth EsjObs.ForecastMeteogramInfo.Obs. data
KambanesE fjordssjObs.Info.Obs. data
KambaskriðurE fjordssjObs.Info.Obs. data
KálfhóllSouthsjObs.ForecastMeteogramInfo.Obs
/weather/stations/
1,9 Mb
2008
Seismic and tsunami early warning activities in Iceland (PDF)
K.S. Vogfjörd, G.G. Pétursson, E. Kjartansson, R. Slunga, K. Ágústsson, S. Hjaltadóttir, G.B. Gudmundsson, M.J. Roberts, H. Geirsson, S. Ármannsdóttir
Poster
12,3
2008
Seismic wave attenuation for earthquakes in SW Iceland - first results (PDF)
Kristján Ágústsson, Bergþóra Þorbjarnardóttir, Kristín Vogfjörð
/earthquakes-and-volcanism/reports-and-publications/
@vedur.is),
P. Crochet, Th. Thorsteinsson, O. Sigurðsson, B. Einarsson
Institute of Earth Science, University of Iceland and DMI
H. Björnsson, S. Guðmundsson, F. Pálsson, G. Aðalgeirsdóttir
Section for Glaciers, Snow and Ice, NVE
L. M. Andreassen, K. Melvold, H. Elvehøy
Uppsala University and Geophys. Inst., University of Alaska
R. Hock, V. Radic
Geocenter Copenhagen, GEUS
A. Ahlstrøm, H
/media/ces/ces_flyer_glacierssnowandice.pdf