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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
2015, 2025, 2035 and 2050
North (Blanda) East (Karahnjukar) South (Thorisvatn)
Change in average inflow to the main storage reservoirs
Watershed
A
v
e
r
a
g
e
i
n
f
l
o
w
[
m
3
/
s
]
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
near the middle of the 21st century
and ∼2–3 ◦C by the end of the century, relative to the 2000–
2009 average. When compared to the reference period 1981–
2000, when the net balance of most of the Icelandic ice caps
was close to zero (Guðmundsson et al., 2011; Aðalgeirsdót-
tir et al., 2006; Guðmundsson et al., 2009b), the temperature
increase is 2.0–2.4 ◦C near the middle of the 21st century
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
for the cases where abstractions and
irrigation are not included (Table 3, top) and included
(Table 3, bottom). The results are spatially averaged, mean
annual values for the 15-year period. The net recharge is
defined as the outflow from the root zone minus the sum of
evapotranspiration and net flow from the groundwater zone
to the overland compartment for the grids where the soil
profile
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
represent annual winter precipitation sums calculatedfrom the stations and multiplied by a constant tuning factor. See Table 3 for explanation of the other runs
Table 3. Correlation (r) and root mean square error (rmse) between modelled and measured winter (bw), summer (bs) and net (bn) balancesat Storbreen. bw-m1: reference modelling bw where Psolid when Tair < 1ºC, bw-m2: Psolid when Tair < 3ºC, bs-m1
/media/ces/GA_2009_91A_4_Andreassen.pdf