on the European level [e.g.
Water Framework Directive (Directive 2000/60/EC),
Common Agricultural Policy, etcetera], except for the
Ukrainian part of the Tisza. However, the Ukraine shows
strong incentives to enter the EU community and thus the
EU acquis communautaire is used as key reference for the
development of its water management principles. It was
nevertheless decided to select two case-studies
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
tg
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to
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orated
:
1:
Ep
ist
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
2015, 2025, 2035 and 2050
North (Blanda) East (Karahnjukar) South (Thorisvatn)
Change in average inflow to the main storage reservoirs
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Last 50 years
Last 20 years
Last 15 years
Last 10 years
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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
thus enabling the delineation of active faults in near-real time. Foreshocks preceding a large
earthquake by more than 20 minutes will already have been located with high precision before
the main shock occurs, and may already have delineated the fault plane of the coming main
shock, thus allowing its faulting mechanism to be immediately inferred. Due to its size, the
main shock
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
Figure 2.3. An overview of the Geysir region. ..................................................................... 20
Figure 2.4 Testing different values for maximum group size in area A1. ............................ 23
Figure 2.5. Testing different values for maximum group size in area A1. ........................... 24
Figure 2.6. A map showing relative locations in box A1 for maximum
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
capability, data interpretation and communication have ad-
vanced with these events. In addition, before the unrest, a variety of
new instruments were installed around the Vatnajökull ice cap by
collaborators in the research project Futurevolc.
During the period of unrest, the Department of Civil Protection and
Emergency Management met regularly with scientists to discuss the
situation
/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