the com-
plexity of the hydrological processes through modelling, but its application is usually limited to
the short-range. Although the results demonstrated a great potential for this method, its success-
ful application in real-time will strongly depend on the quality and availability of streamflow
observations, which can be poor or simply missing during periods of variable durations, e.g
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.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
***
(0.637) (0.638)
Contribution of the first mover −0.040**
(0.020)
No. observations 1180 1180
Prob > χ2 0.0000 0.0000
Wald χ2 48.51 52.26
Log Likelihood 439.69 437.63
same contribution as the first mover, was chosen to keep the design simple and to identify
types. Only advantageous inequity aversion should affect second movers’ decisions.
The number of times that second movers match the public good
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
discharge versus deterministic forecast over the period 01/09/2001–
31/08/2005. The solid line corresponds to a perfect match. For methods 1 to 4,
rescaling is applied. ...................................................................................... 31
5
6
1 Introduction
The Icelandic Meteorological Office (IMO) is responsible for the hydrological monitoring and
issuance of flood warnings
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
principles would often not
match up exactly, as happenend with the steps, we
reconstructed seven “umbrella principles.” Under
each of these, we listed a number of similar
principles in a principles summary table (Appendix
4: Table A4). We discussed the meaning of each
umbrella principle and the comparison of its
underlying principles from the four guides in the
right-hand column, as well as agreement
/media/loftslag/vonKorff_etal-2010.pdf
of events closely.
Photo: Sigurlaug Gunnlaugsdóttir.
Bárðarbunga
Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com-
munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson.
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
5
The magma intrusion from Bárðarbunga
to the eruption site at Holuhraun and
related tremor pulses
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
the lightning cluster 10‒20 km to the north. The same wind correction as
applied for 2011 moves the eruption site estimate to about 4 km WNW of the correct site. By
applying a smaller wind correction (time constant of 200 s instead of 500 s) gives a perfect
match for Eyjafjallajökull for the day with the highest frequency of volcanic lightning (16
May 2010).
13
Figure 7
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf