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
the Fljótsdalsheiði region . . . . . . . 47
18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48
19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49
20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50
21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51
22 Seasonal mean
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.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
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
–8% likelihood that a vent will open on Heimaey. In other words, there is a 92–97% likelihood
that the next eruption within the volcanic system will not be on Heimaey. The most densely
populated parts of Heimaey in the north and around the harbor are the most vulnerable to
Moderate and Large lava flows originating on the island. Almost all infrastructure on the island
is vulnerable to lava
/media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
in glacial hydrology in Iceland ............................................................................................. 92
CLIMATE CHANGE EFFECTS ON RENEWABLE ENERGY
Fidje, A., Seljom, P., Rosenberg, E., Haugen, J.E., Meir, M., Rekstad, J. and Jarlset, T.
Impacts of climate change on the Norwegian Energy System towards 2050 ........................................................ 94/media/ces/ces-oslo2010_proceedings.pdf