Advantageous inequity aversion plays
no role for first-movers’ decisions as they cannot earn more than second movers.
We assume that risk aversion and inequity aversion are independent.7 Therefore, the ex-
pected utility of agent i in the role of the first mover is the sum of her expected utility with
respect to her own gain and her expected utility related to the second mover’s gain:
EUi1 =Evi1( ˜Xi1
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
108 Reykjavík
Sara Barsotti, Veðurstofa Íslands
Sigrún Karlsdóttir, Veðursstofa Íslands
Anna María Ágústsdóttir, Landgræðslan
Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra
Íris Marelsdóttir, Embætti landlæknis
Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans
Þórólfur Guðnason, Embætti landlæknis
Bogi B. Björnsson, Veðurstofa Íslands
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
) undirbúning rauntíma-
kortlagningar á eftirskjálftavá, og 6) rauntímakortlagningu spennuútlausna skjálfta.
Upplýsingar um SAFER verkefnið má finna á vefsíðunni: http:// www.saferproject.net/.
7
Contents
List of figures ........................................................................................................................... 7
List of tables
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
type, surface condition and weather
was noted. In total more than 100 point measure-ments were made during three days (2 and 3 August2006 and 7 August 2007). Measurements weremade on different surface types: ice, snow and firn,
as well as on different surface conditions (dry, wet,clean, dirty). Some of the measurements will be re-ferred to in this paper.
Meteorological observations outside
/media/ces/GA_2009_91A_4_Andreassen.pdf
/CES_D2.4_task1.html
2
Table of Contents
Abstract 1
1. Introduction 2
2. Methods and data sets 5
3. Results for temperature 7
4. Results for precipitation 14
5. Tables for individual locations 19
6. Summary 24
Appendix: details of methodology 26
A.1 Data sets 26
A.2 Derivation of regression coefficients 27
A.3 Smoothing of the probability distributions 30
References 31
/media/ces/CES_D2.4_task1.pdf
by an approximately 70 km long and 15 km wide left lateral shear zone, the
South Iceland seismic zone (SISZ). Approximately every 100 years a sequence of large
earthquakes of magnitudes M 6-7 occurs in the zone and traces of many Holocene faults
have been mapped on the surface. Although the trend of the zone is east-west, major
earthquakes take place on north-south striking faults, which leads
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
judgment and statistical analysis of a body of evidence (e.g. observations
or model results), then the following likelihood ranges are used to express the assessed probability of occurrence: virtually certain >99%;
extremely likely >95%; very likely >90%; likely >66%; more likely than not > 50%; about as likely as not 33% to 66%; unlikely <33%; very
unlikely <10%; extremely unlikely <5
/media/loftslag/IPPC-2007-ar4_syr.pdf
February, March-April-May and the overview article (list of links).
Calendar
Below is a calendar with a short-cut to each day of this month's events:
Sept.:1-2-3-4-5-6-7-8-9-10-11-12-13-14-15-16-17-18-19-20-21-22-23-24-25-26-27-28-29-30
Panoramic view towards the eruptive site in Holuhraun 3rd September 2014. Photo: Richard Yeo.
Updated information
30 September 2014 18:50 - from
/earthquakes-and-volcanism/articles/nr/3001
February, March-April-May and the overview article (list of links).
Calendar
Below is a calendar with a short-cut to each day of this month's events:
Sept.:1-2-3-4-5-6-7-8-9-10-11-12-13-14-15-16-17-18-19-20-21-22-23-24-25-26-27-28-29-30
Panoramic view towards the eruptive site in Holuhraun 3rd September 2014. Photo: Richard Yeo.
Updated information
30 September 2014 18:50 - from
/earthquakes-and-volcanism/articles/nr/3001/