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Organisers
NONAM
•Finnish Meteorological Institute, FMI (Adriaan Perrels)
•Geological Survey of Denmark and Greenland, GEUS (Jens
Christian Refsgaard and Hans Jørgen Henriksen)
•Icelandic Meteorological Office, IMO (Sigrún Karlsdóttir)
FIVA - International Research School of Water
Resources
•University of Copenhagen, KU (Frederik Uldall)
Course objectives
• To introduce students to the concept
/media/loftslag/Refsgaard_1-Welcome.pdf
ilmiö
W inter Sprin g
SummerA utumn
Kosteus
Lauha t talve t
Talvitulvat
Jäätävä sade
Hyyde
Kova tuu li
…
Aikaisempi
kevät ja tu lvat
Ku ivuus
Ku ivuvat
vesiva rastot
…
Ku ivuus
Rankkasa teet
sa lamointi
Rakeet
…
Myrskyt
Rankkasateet
Rou ta
Jääkannen
muodostaminen
…
yli y €yli y €Merkittävät3
x - y €x – y €Keskinkertaiset2
alle x €alle x €Vähäiset1
Mahdollisuuden
tunnisteväriRiskin
/media/ces/Keranen_Jaana_CES_2010.pdf
Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009
ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost
operating manage- ment develop- poned-, of land grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation
/media/loftslag/Traffc-maintenance_expenditures.pdf
/lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13
April 2009.
[2] WTO, World Tourism Organization (2008): “Climate Change and Tourism -
Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain.
Available at:
http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7
March 2010.
[3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for
sustainable
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.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