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to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
(-33%) during 1970 to 2004 has been smaller than the com-
bined effect of global income growth (77%) and global population
growth (69%); both drivers of increasing energy-related CO2 emis-
sions. The long-term trend of declining CO2 emissions per unit of en-
ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM}
Differences in per capita income, per capita emissions and
energy
/media/loftslag/IPPC-2007-ar4_syr.pdf
SE +56:52:00 +14:48:00 166 TP
2 FALUN SE +60:37:00 +15:37:00 160 T
4 LINKOEPING SE +58:24:00 +15:31:59 93 T
5 LINKOEPING-MALMSLAETT SE +58:24:00 +15:31:59 93 T
8 OESTERSUND SE +63:10:59 +14:28:59 376 T
9 OESTERSUND-FROESOEN SE +63:10:59 +14:28:59 376 T
10 STOCKHOLM
/media/ces/CES_D2.4_task1.pdf
. . . . . . . . . . . 56
27 Directional mean wind power density within the Langanes region . . . . . . . . . . 57
28 Seasonal mean wind power density within the Langanes region . . . . . . . . . . . 58
29 Directional mean wind power density within the Meðallandssveit region . . . . . . 59
30 Seasonal mean wind power density within the Meðallandssveit region . . . . . . . 60
31 Directional mean
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
). It was widely felt in the capital area and in Akranes. Another magnitude 3.1 event was measured earlier the same day at 11:58 at the same location. Hypocenter depths of the earthquakes were around 3-4 km.
This earthquake sequence started in the morning around 10:00 and so far more than 100 events have been detected. Focal mechanisms of the largest events show normal faulting movements (vertical
/about-imo/news/nr/3138
in Reykjavík
6.3.2013
As everyone is aware of, very bad weather is prevalent in all of the country. Reykjavík is unusually hard hit by winds and snow. Following is the weather forecast, issued at 15:58, but users of the web are advised to observe the frequently updated maps
/about-imo/news/nr/2665
by
rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com-
mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target
site:
bQi(D;T ) = µi(D)qR(D;T ); (1)
where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged
over duration D, at site i. The regional growth curve, qR(D;T
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
level, surveys commissioned by the European Com-
munity/the European Union provide an indication of trends in concern about cli-
mate change. Since 1992, such surveys have been undertaken among representative
samples of citizens in its Member States, and specifically on topics related to the
environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB
in 2002). These have included
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
accumulation rate on the ground on 21 September 1983 (Hekla) ............... 57
Figure 31 Tephra accumulation rate on the ground on 9 June 1986 (Hekla) ........................... 58
Figure 32 Tephra accumulation rate on the ground in Geysir (Hekla) .................................... 59
Figure 33 Event Tree for Katla volcano
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf