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grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation velopment
Mainten- Cons- life cycle according Fund in the
ance 1960- truction financial to the structural fund
1990 1960- projects Road programmes
1990 Act1) of the EU
Expenditure of Finnish Road Administration in 1960 - 2009
1 000 e
1980 42 409 153 761 14
/media/loftslag/Traffc-maintenance_expenditures.pdf
2015, 2025, 2035 and 2050
North (Blanda) East (Karahnjukar) South (Thorisvatn)
Change in average inflow to the main storage reservoirs
Watershed
A
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e
r
a
g
e
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n
f
l
o
w
[
m
3
/
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]
0
2
0
4
0
6
0
8
0
1
0
0
1
2
0
Last 50 years
Last 20 years
Last 15 years
Last 10 years
Last 5 years
Temperature corrected
Transformation of climate measurements
•Change in temperature
• 0.75 °C/100y 1950-1975
• 1.55
/media/ces/Linnet_Ulfar_CES_2010.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
in Askja
8 Projects
9 The weather in Iceland 2014
10 Finance
11 Sta?publications
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
3
One of the main goals of the merger of the Hydrological Service,
HS, and the Icelandic Meteorological O?e, IMO, was to improve
the capabilities regarding monitoring, warnings and emergency
response due to natural hazards. Prior
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
up to ~13 km height.
BY K. S. VOGFJÖRD, S. S. JAKOBSDÓTTIR,
G. B. GUDMUNDSSON, M. J. ROBERTS, K. ÁGÚSTSSON,
T. ARASON, H. GEIRSSON, S. KARLSDÓTTIR,
S. HJALTADÓTTIR, U. ÓLAFSDÓTTIR,
B. THORBJARNARDÓTTIR, T. SKAFTADÓTTIR,
E. STURKELL, E. B. JÓNASDÓTTIR, G. HAFSTEINSSON,
H. SVEINBJÖRNSSON, R. STEFÁNSSON, AND T. V. JÓNSSON
Research, 2005), which are complemented by
three continuous GPS stations
/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
Refsgaard a,*, Jeroen P. v
Peter A. Vanroll
a Geological Survey of Denmark and Greenlan
b Copernicus Institute for Sustainable Development and Innovation
Utrecht University, Utrecht
c
Environmental Modelling & Softwar
equitable manner without compromising the sustainability of
* Corresponding author. Tel.: þ45 38 142 776; fax: þ45 38 142 050.
E-mail address: jcr@geus.dk (J.C. Refsgaard).
1364-8152
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
Annual
report
? Icelandic Met O?e
Bústaðavegur –
Reykjavík
Iceland
Editors:
Sigurlaug
Gunnlaugsdóttir
Sigrún Karlsdóttir
Ingvar Kristinsson
Theódór F. Hervarsson
Design and layout:
Vinnustofa
Atla Hilmarssonar
Printing:
Oddi
Cover photo:
Oddur Sigurðsson
ISSN -
The Icelandic Meteorological O?ce, IMO, is responsi -
ble for real-time monitoring and forecasting
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
-
charge, the RMS values are calculated as in equation (8). An
RMS value of 0 implies a perfect match between simulated
and observed values. The RMS value increases with the
discrepancy between the simulated and observed values.
[38] At the downstream discharge stations of the three
stream systems an average value of E = 0.81 and RMS =
1.84 m3/s was found for the validation period 1996–1999
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf