and the geographic extent of Figure 1b. Except where indicated, all networks are operated by
IMO, which displays data in real-time at http://www.vedur.is/english/. (b) Map of the Vat-
najökull ice cap, showing the 1 November 2004 eruption site and located earthquakes in the
month preceding the eruption. Epicenters in Skeidarárjökull outlet glacier represent icequakes
induced by the jökulhlaup
/media/jar/myndsafn/2005EO260001.pdf
HYDROPOWER IN ICELAND
Impacts and adaption in future climate
Authors
Óli Grétar Blöndal Sveinsson (Phd)
Úlfar Linnet (MSc)
Elías B. Elíasson (MSc)
Landsvirkjuns system
•Installed power 1850 MW
• 96 % Hydroelectricity
• 4% Geothermal
•Production capacity 13 TWh/a
•Customer base
• 86 % Large industries
• 14 % Small businesses / Household
•No connection to other countries
•Reliability a major
/media/ces/Linnet_Ulfar_CES_2010.pdf
scenario Summer Winter
Temp ▲6˚c ▲7˚c.
Precip. +10% +30%
CO N l d bl2 ear y ou e
11
Forest management principles
1
)
Basal area just
before thinning
Thinning threshold
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B
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a
Basal area just
Remaining basal
area threshold
Dominant height (m)
after thinning
12
Management regimes
Changes in basal area thinning thresholds
/media/ces/Alam_Ashraful_CES_2010.pdf
/EPP 2
Stakeholders analysis
26 August 2011 PM/YZ/EPP 3
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/media/loftslag/Group5-Stakeholders_involvement.pdf
). Locations of the weather sta-
tions, used to reconstruct the temperature and precipitation records,
are shown with letters: Reykjavík (R), Fagurhólmýri (F), Hæll (H),
Stykkishólmur (S), Teigarhorn (T), Vestamannaeyjar (V), Akureyri
(A) and Hólar in Hornafjörður (HH). (B) The surface topography of
Vatnajökull ice cap. Dots show the sites of mass balance and veloc-
ity measurements, blue dots show
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
and Implementation of Seismic Early Warning Processes in South-West Iceland
Kristín S. Vogfjörd, Einar Kjartansson, Ragnar Slunga, Páll Halldórsson, Sigurlaug Hjaltadóttir, Gunnar B. Gudmundsson o.fl.
83 bls.
3,2 Mb
2010-003
Use of relatively located microearthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir
104
/earthquakes-and-volcanism/reports-and-publications/
frequency distributions for Re-
gion 1 derived with index flood model no. 6: bµ(D) = a(AP=Z)b ............................ 39
5
Appendix VI - Empirical and modeled daily flood frequency distributions for
Region 2 derived with index flood model no. 3: bµ(D) = a(APm)b ......................... 41
Appendix VII - Instantaneous Index flood models for Region 1. .......................... 43
Appendix VIII
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
= {0, . . . ,20}. The second option, option b, is
such that the dictator keeps 18 points for herself and gives two points to the receiver: the
distribution (18,2). In decision 1, the dictator thus chooses between the distribution (0,0)
(zero for herself and zero for the receiver) and the distribution (18,2) (18 for herself and
two for the receiver); in decision 2, the choice is between (1,1
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf