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/weather/stations/
CMIP3 Multimodel Dataset: A New Era in Climate
Change Research. Bulletin of the Americal Meteorological Society, 88, 1383-1394.
Naki enovi , N. and R. Swart (Eds.) 2000: Emission Scenarios. A Special Report of Working
Group III of the Intergovernmental Panel on Climate Change. Cambridge University Press,
599 pp.
Räisänen, J. and L. Ruokolainen 2006: Probabilistic forecasts of near-term climate
/media/ces/CES_D2_2_poster_3x3.pdf
and distribution network are all identified
a section at a time. In some cases, however, it might
be more valuable to focus only on a certain part of
functional model.
Fig.1. Functional Model.
The results of the risk analysis are represented
visually in a fourfold table. (Fig.2) The main idea of the
table is to provide a readily interpretable overview of
h hi hli h d i k d i i i l i
Having already been
/media/ces/ces_risk_flyer.pdf
-OBS data set (ver. 1.1) (Haylock et al., 2008)
Data and method
Variables (daily)
max and min 2m temperature
max 10m gust wind (Brasseur 2001 )
accumulated precipitation
Extreme events
the generalised extreme value (GEV) distribution
the 20-year return values of
annual max/min temperature and max gust wind
summer and winter maximum of precipitation
fitting the GEV: stationary model, L-moments
/media/ces/Nikulin_Grigory_CES_2010.pdf
for
behavioural responses to policy
• Psychological models of behaviour change (e.g., TPB)
Ajzen & Fishbein (1991)
Subjective
norm
Specific
attitudes
Perceived
behavioural
control
Intention Behaviour
Normative
beliefs
Behavioural
beliefs
Control
beliefs
P
O
L
I
C
Y
(3) Factors important for
behavioural responses to policy cont.
• Cost-minimization principle (Loukopoulos et al. 2006)
• Barriers
/media/loftslag/Eriksson_2-Acceptability-of-policy.pdf
Use of relatively located micro-
earthquakes to map fault patterns
and estimate the thickness of the
brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir
VÍ 2010-003
Skýrsla
f lll dUse o re ative y ocate micro-
earthquakes to map fault patterns
and estimate the thickness of the
brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir, Veðurstofu Íslands
VÍ 2010-003
ISSN 1670-8261
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
in Finland
Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b
a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland
b Department of Geography, FI-20014 University of Turku, Turku, Finland
a r t i c l e i n f o
Article history:
Received 7 January 2010
Received in revised form 13 June 2010
Accepted
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
at the bound-
aries. With longitude, l , parameterised as a function of latitude, f , these boundaries are at
l1 = 30
30
40
(f 40) (2)
and
l2 = 45
90
40
(f 40) : (3)
This suggests dividing the study domain into three parts: a western sector, with l < l1, covering
the region west of Greenland; a central sector, with l1 l < l2, including the region of the
Icelandic Low; and an eastern sector
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf