+2αi )1+αi )
1−ri + (1 − pi1)(10 + 0.6xi1)1−ri
1 − ri
(11)
The first mover’s beliefs about the second mover’s type, i.e., the second mover’s β , and her
risk aversion both affect the optimal contribution. Depending on the second mover’s choice,
the first mover may earn the same as or less than the second mover. Regarding inequity
preferences, only the first mover’s disadvantageous inequity aversion
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
m
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/media/ces/2010_017.pdf
Extreme precipitation in Iceland: Climate
projections and historical changes in
precipitation type
Andréa-Giorgio R. Massad
Guðrún Nína Petersen
Halldór Björnsson
Matthew J. Roberts
Tinna Þórarinsdóttir
VÍ 2022-006
Skýrsla
Extreme precipitation in Iceland: Climate
projections and historical changes in
precipitation type
Andréa-Giorgio R. Massad
Guðrún Nína Petersen
Halldór Björnsson
Matthew
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
2012).
This project aims at investigating and quantifying hazard at the ground due to tephra
released during explosive eruptions in Iceland. Hazard and potential impact are assessed
for selected eruption scenarios.
Table 1. List of scenarios that have been investigated in this project. — Sviðsmyndir sem
notaðar eru við hermanir og útreikninga.
Scenario Eruption type Volcanic
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
) and changing climate (CC:CC)
1. Current climate (CU)
- varying thinning regimes
(0%, 15%, 30%,45%)
2. Changing climate (CC)
- varying thinning regimes
(0%, 15%, 30%,45%)
3. Current (CU) &
changing climate (CC)
- current thinning regime
4. Current (CU) &
changing climate (CC)
- changed thinning regimes
C
l
i
m
a
t
e
s
c
e
n
a
r
i
o
s
M
ea
s
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r
e
m
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t
s
o
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p
/media/ces/CES_BioFuels_Flyer_new.pdf
we take the corresponding
data from the CMIP5 project.
Table 1. All GCMs and RCMs used in this study. If a model is available for any of the
domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is
unavailable.
Model name Type EURO-11 EURO-44 Arctic-44
CCCma-CanESM2 GCM x v v
COSMO-CLM4-8-17 RCM v v x
CNRM-CERFACS-CNRM-CM5 GCM v v x
IHCEC-EC-Earth GCM v v v
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
;script type="text/javascript" src="http://vedur.is/js/iframe.js"></script>
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To show other areas, a different digit must be entered after 'Vi.ifrm.area'. The area codes are as follows:
101 = whole country
111
/about-imo/the-web/iframes/wind-temp-precip/
be copied to your html file where the frame should appear:
<script type="text/javascript" src="http://vedur.is/js/iframe.js"></script>
<script type="text/javascript"><!--
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VI.ifrm.area = 101;
VI.ifrm.lang = 'en';
VI.ifrm.displayWeather();
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</script>
To show other areas, a different digit must be entered after 'Vi.ifrm.area
/about-imo/the-web/iframes/wst-txt-obs/
Steinunn S. Jakobsdóttir & others - Opening address
08:55 Ragnar Stefánsson - From earthquake prediction research to useful warnings ahead of earthquakes
09:20 Ragnar Slunga - Microearthquakes, stresses, crustal stability, and earthquake warnings
09:45 Reynir Bödvarsson - Development history and future potential of the SIL system
10:10 Coffee and posters
10:50 Halldór Geirsson & others
/earthquakes-and-volcanism/conferences/jsr-2009/schedule/
Infrasonic and Seismic Signatures of the 2014 Askja Landslide
Giulia Barfucci¹, Maurizio Ripepe¹, Giorgio Lacanna¹, Emanuele Marchetti¹,
Kristín Jónsdóttir², Kristín S. Vogfjörð²
(1) Department of Earth Sciences, University of Firenze, via LaPira, 4, 50121 Firenze, Italy
(2) Icelandic Meteorological Office, Reykjavik, IS-108, Iceland
Landslides commonly occur at active volcanoes and represent
/media/norsem/norsem_giulia.pdf