behavior as the models we would like to compare it with – Campbell,
Joyner and Boore, and Fukushima and Tanaka–despite the generally lower predictions.
Campbell's model is only valid for distances less than 50 km since his data set, of magnitude 5
to 7.7 events, consisted only of observations close to the epicenter (more than 86% were closer
than 30 km).
The theoretical relation for attenuation
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
(97%)
relative to maritime storms decreases. This relative and absolute increase in the occurrence of
maritime cyclones in the central sector, with increasing time-scale, emphasises again the cli-
matological significance of the Icelandic Low. During summer, the cyclone density over land
increases on all time-scales and in each sector, compared with winter. There is also a relative
increase
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.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
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
Berthier3
1Institute of Earth Sciences, University of Iceland
2The Icelandic Meteorological Office
3Centre National de la Recherche Scientifique, Laboratoire d’Etudes en Géophysique et Océanographie
Spatiale, Université de Toulouse, France
* Corresponding author, e-mail: sg (at) hi.is
ABSTRACT
We assess the mass balance changes of the ~81 km2 Eyjafjallajökull ice cap in South Iceland,
over three
/media/vatnafar/joklar/Reykholt-abstracts.pdf
2006),
as well as the fault of a M 4.6 earthquake near to the station kri in March 2006.
27
Figure 3. (Upper) A map showing the Hengill- and Ölfus test area. (Lower) A vertical
cross section, viewed from the south. Pink circles show the 1997–98-library events,
orange circles show library events from 2000 and green circles show 2008-library
events. The red stars show location of two M>5
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
on the European level [e.g.
Water Framework Directive (Directive 2000/60/EC),
Common Agricultural Policy, etcetera], except for the
Ukrainian part of the Tisza. However, the Ukraine shows
strong incentives to enter the EU community and thus the
EU acquis communautaire is used as key reference for the
development of its water management principles. It was
nevertheless decided to select two case-studies
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
and Jónsson, S.
Importance of groundwater modelling in hydrological modelling in Iceland and implementation of the
groundwater module in the hydrological model WASIM for two water sheds in Iceland .................................... 84
Einarsson, B. and Jónsson, S.
The effect of climate change on runoff from two watersheds in Iceland .............................................................. 86/media/ces/ces-oslo2010_proceedings.pdf