Evaluation of HARMONIE reanalyses of
surface air temperature and wind speed
over Iceland
Nikolai Nawri
VÍ 2014-005
Skýrsla
2
Evaluation of HARMONIE reanalyses of
surface air temperature and wind
speed over Iceland
VÍ 2014- 005
ISSN 1670- 8261
Skýrsla
+354 522 60 00
vedur @vedur . is
Veður st of a Íslands
Búst aðaveg ur 7 – 9
108 Reyk j avík
Nik olai Nawr i
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
................................................................................................................... 8
Liss M. Andreassen, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen ..................... 9
Lidar measurements of Norwegian glaciers – an overview
Neil Arnold* and Gareth Rees .............................................................................................. 10
Calculation of glacier velocity from repeat
/media/vatnafar/joklar/Reykholt-abstracts.pdf
00
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
108 Reykjavík
Guðrún Elín Jóhannsdóttir, Department of Earth Sciences at Uppsala University
Abstract
Flood risk increases with rising sea levels and coastal settlements need to adapt to this increasing
risk. For that, hazard and risk assessments are an important step. Coastal floods have caused prob-
lems in Iceland in the past
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
; fax: +358 20 490 2590.
E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen).
Journal of Hydrology 391 (2010) 333–350
Contents lists available at ScienceDirect
Journal of Hydrology
journal homepage: www.elsevier .com/ locate / jhydrol
Author's personal copy
narios from GCMs or RCMs, and with different emission scenarios
(e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
construction and maintenance.
7. Path dependency, meaning that roads will likely continue to exist even if the
underlying need for them decreases.
8. Social shifts, personal ownership of cars no longer seen as necessary. Car-sharing
becomes part of a suite of mobility options within the collective transportation
system.
9. Behavioral shifts, mobility no longer dominant variable in daily life
/media/loftslag/Group4.pdf
ANNUAL REPOR T 2014
2
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
?Veðurstofa Íslands 2015
Bústaðavegur 7–9, 108 Reykjavík, Iceland
The annual report was drafted by the IMO sta?.
Editor: Sigurlaug Gunnlaugsdóttir
Design and layout: Hvíta húsið
Printing: Oddi
ISSN 2251-5607
Cover photo: Gro Birkefeldt Møller Pedersen
I N D E X
4 Bárðarbunga
7 Rockslide
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
-corrected SPOT 5
high-resolution geometric (HRG) images with 2.5 m
2.5 m spatial resolution, acquired in the autumn 2003
and (4) airborne polarimetric synthetic aperture radar
images observed simultaneously to the 1998 EMISAR
images and the EMISAR DEM viewed as a shaded
relief image (Magnu´sson et al. 2005b).
We estimate the average specific net mass balance (in
m yr1 w. eq.) as
bn r
DV
A1 N
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
of communication. However, it could be
9
improved e.g. by making it more simple and easy to grasp. The list of publications is
important, but at present the publications cannot be downloaded. A future improvement
would be to have a list of downloadable publications. A substantial improvement would be
executive summaries of publications adapted for stakeholders. Fact sheets could be an
important
/media/ces/ces-oslo2010_proceedings.pdf
and our intention is to run these models dur-
ing times of hazardous events and even on a daily
basis to further improve monitoring.
Avalanche monitoring has progressed. The em-
phasis is now on improving our services, especially
to the Icelandic Road and Coastal Administration
with regard to transport. The reason is that com-
munity structure has changed considerably in recent
years and the need
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
bursts of
seismic tremor (1–3 Hz), and later becoming
periodic with energy between 2 and 8 Hz. After
18 October, seismicity increased to three events
per day (Figure 2b). Synchronous with this
increase, the ISGPS station SKRO (Figure 1b)
moved 9 mm westward over the following eight
days, and returned to its original position on 1
November (Figure 2c), suggesting subsurface
magma movement
/media/jar/myndsafn/2005EO260001.pdf