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
would lead to a reduction of 20%
of total annual tourist flow to Spain between 2004 and 2080; Hein, Metzger and Moreno
[9] obtain an average decrease up to 14% in 2060 compared to 2004 - result of higher
losses in summer and slight increases in the remainder of the year-.
Nevertheless, some studies offer a more positive outlook. According to the Fundación
Empresa y Clima [7], the tourist
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
-
corded and important data on the deformation of the caldera ac-
quired.
The real-time monitoring and interpretation of geophysical data
were made accessible to the public via the internet. Both automatic
and manually checked earthquake locations were displayed on
maps, updated every five minutes. Also, cGPS time series were
mapped showing deformation in the area.
Scientists followed the course
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
(). The circulation of Icelandic waters-a
modelling study. Ocean Science , –.
Nygaard, B. E. K., Hálfdán Ágústsson & K.
Somfalvi-Toth (). Modeling wet snow ac-
cretion on power lines: improvements to previ-
ous methods using years of observations.
Journal of Applied Meteorology and Climatology
(), –.
Philippe Crochet (). Sensitivity of Icelandic
river basins to recent
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
in global
terrestrial biosphere models. About 20 sci-
entists from the crop modeling and global
biosphere modeling community attended. The
workshop was one in a series of workshops
sponsored by Quantifying and Understanding
the Earth System (QUEST), a program of the
U.K. Natural Environment Research Council
(NERC). QUEST has several activities, among
them the focused strategic activity
/media/jar/myndsafn/2005EO260001.pdf
Numerical simulations
of precipitation in the complex terrain of Iceland—Comparison with glaciolog-
ical and hydrological data. Meteorol. Z., 16(1), 71–85.
Rögnvaldsson, Ó. and Ólafsson H. 2008. Dynamical downscaling of precipi-
tation – Part I: Comparison with glaciological data. Proceedings of the XXV
Nordic Hydrological Conference, Reykjavík, Iceland.
Tómasson, H. 1982. Vattenkraft i Island och dess
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
Discrete
numerical
Categorical Narrative
Constant in space and time A1 A2 A3
4Varies in time, not in space B1 B2 B3
Varies in space, not in time C1 C2 C3
It is noticed that the matrix is in reality three-dimensional
(source, type, nature). Thus, the categories type and nature
are not mutually exclusive, and it may be argued that the ma-
trix should be modified in such a way that the two uncer
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
and Irrigation
Current climate 560 23 264 243 10 18
A2 scenario + 74 (13%) 0 + 50 (19%) 0 0 + 16 (89%)
B2 scenario + 118 (21%) +1 (4%) + 84 (32%) + 20 (8%) 0 + 9 (50%)
aWater balance values are in millimeters. Relative changes are in parentheses.
Table 4. Spatially Averaged, Mean Monthly Recharge for the
Current Climate and the A2 and B2 Scenarios for the Simulation
Without Abstractions
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf