........................................................................................................................... 3
Summary ............................................................................................................................... 4
Summary of the break-out sessions on road infrastructure ................................................... 6
Summary of the break-out sessions on Horsens case
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
and local planners, business strategists
and risk managers and policy-makers as well as representatives of NGO’s and Nordic/
international organizations. While some sessions will have a definite Nordic focus, the confer-
ence - just like the field of climate change adaptation is by no means restricted to the Nordic
region. We cordially invite and strongly encourage international participants
/media/loftslag/myndasafn/Nordic_Adaption_14_2cir.pdf
(see below) and the list of participants in addition to the abstracts of presentations and posters.
Sessions
Thursday, 20 June
09:00–09:10 ‒ Welcome
09:10–10:30 ‒ Lidar measurements for glacier inventories and mass balance monitoring
11:00–12:30 ‒ Process studies – I
13:30–15:00 ‒ Process studies – II
15:30–17:30 ‒ Lidar measurements from space, incl. video discussion with input from NASA
/lidar/lidar-2013/program/
students’ application forms. The provided knowledge will also be of use in the review sessions and the
linking tasks for the Conference.
Early August suggested literature will be put on the NONAM website. You will be notified about uploads.
Review sessions
The backbone of the PhD Workshop consists of three sets of five parallel review discussion sessions. In each
parallel session a topic
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
of events closely.
Photo: Sigurlaug Gunnlaugsdóttir.
Bárðarbunga
Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com-
munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson.
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
5
The magma intrusion from Bárðarbunga
to the eruption site at Holuhraun and
related tremor pulses
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.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
level in Skeidará waned. The last sign of a
crater explosion was seen at GRF early on 6
November, leaving only a weak tremor signal
from the remnants of the jökulhlaup. The
jökulhlaup fi nally ended in early December,
after ~0.8 km3 of water had drained from the
Grímsvötn lake (J. Hardardóttir, personal com-
munication, 2005).
Location and Volume Constraints
Earthquake locations at Grímsvötn
/media/jar/myndsafn/2005EO260001.pdf
a systematic com-
parison of results to observed precipitation has been carried out. Un-
dercatchment of solid precipitation is dealt with by looking only at
days when precipitation is presumably liquid or by considering the
occurrence and non-occurrence of precipitation. Away from non-
resolved orography, the long term means (months, years) of observed
and simulated precipitation are often
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
and possibly the stake-
holders at different phases of the modelling project.
Many QA guidelines exist such as Middlemis (2000) and
Van Waveren et al. (1999). The HarmoniQuA project (Schol-
ten et al., 2007; Refsgaard et al., 2005a) has developed a com-
prehensive set of QA guidelines for multiple modelling
domains combined with a supporting software tool, MoST
(downloadable via http
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf