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
magnitudes. (b) Seismic tremor amplitude in three different frequency bands. (c) Volcanic plume
height. (d) Number of lightning. Lightning and tremor amplitude roughly correlate with plume
height.
Intensifi ed human activity and a growing
population have changed the climate and the
land biosphere. One of the most widely recog-
nized human perturbations is the emission of
carbon dioxide (CO2
/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
BIOMATH, Ghent University, Gent, Belgium
d Water Quality Modelling modelEAU, University Laval, Quebec, Canada
Received 20 December 2005; received in revised form 5 February 2007; accepted 7 February 2007
Available online 27 April 2007
Abstract
A terminology and typology of uncertainty is presented together with a framework for the modelling process, its interaction with the broader
water
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
and Irrigationa
Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Current 101 85 59 13 6 4 1 6 39 79 8497
A2 145 132 73 10 10 7 6 8 4 75 92 123
B2 137 119 75 16 6 6 6 5 21 74 110 141
aValues are in millimeters.
10 of 18
W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15
time and larger area where groundwater levels rise above
the drain levels. Table 6 shows the mean discharges
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf