will review a set of stakeholder involvement and
decision making issues with the above outline as backdrop.
References:
[1] Marttila, V., Granholm, H., Laanikari, J., Yrjölä, T., Aalto, A., Heikinheimo, P., Honkatukia, J., Järvinen,
H., Liski, J., Merivirta, R. & Paunio, M. 2005. Finland’s National Strategy for Adaptation to Climate Change.
MMM Publication 1a/2005. 276 pp.
[2] Kokkarianen, V/media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf
(-33%) during 1970 to 2004 has been smaller than the com-
bined effect of global income growth (77%) and global population
growth (69%); both drivers of increasing energy-related CO2 emis-
sions. The long-term trend of declining CO2 emissions per unit of en-
ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM}
Differences in per capita income, per capita emissions and
energy
/media/loftslag/IPPC-2007-ar4_syr.pdf
and our intention is to run these models dur-
ing times of hazardous events and even on a daily
basis to further improve monitoring.
Avalanche monitoring has progressed. The em-
phasis is now on improving our services, especially
to the Icelandic Road and Coastal Administration
with regard to transport. The reason is that com-
munity structure has changed considerably in recent
years and the need
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
In Chapter 3 we focus on the following monthly averages: Near-surface 2 meter temperature
(TAS), total precipitation (TP), and sea ice cover (SI). In Chapter 4 we add surface air
pressure (PSL) and snow cover thickness (SNCT). The following daily fields will be studied
as well: Near-surface wind speeds, (U and V sfcWind), maximum near-surface 2 meter
temperature (TASMAX), minimum mean-surface 2 meter
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
14 0 1 2 3 8 12
15 0 1 2 3 8 12
16 0 1 2 4 8 12
17 0 1 2 4 8 12
18 0 1 2 4 8 12
19 0 1 2 4 8 13
20 0 1 2 4 8 13
21 0 2 3 5 9 13
22 1 2 3 5 9 13
23 1 2 3 4 9 13
MEAN 1 2 2 4 8 13
10
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:2001–201
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:6
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59’06"
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LONGITUDE
:2
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36’20"
W
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V
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MSL
:5
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/media/vedur/aerodrome_summaries_20140603.pdf
tunnisteväriSeuraukset
Scenario probability high
ACT
MONITOR
Consequence
probabi lity low
after control
methods
PREPARE
PREPARE
Scenario probability low
Consequence
probabili ty high
after control
methods
Likely
Very unl ikely
Very likely
Virtuall y certain
Unlikely
V
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Excepti onally unlikely
= major consequences
= moder ate consequences
= minor
/media/ces/Keranen_Jaana_CES_2010.pdf
course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
……………………………………………………………………………………………………………………………………………………………………
6
Figure 1. Flow chart summarizing information and decision flows of an adaptive management inspired
adaptation planning cycle for road transport (at national strategic / tactical level)
M
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/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
; fax: +358 20 490 2590.
E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen).
Journal of Hydrology 391 (2010) 333–350
Contents lists available at ScienceDirect
Journal of Hydrology
journal homepage: www.elsevier .com/ locate / jhydrol
Author's personal copy
narios from GCMs or RCMs, and with different emission scenarios
(e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
with 20% and 2% for the HIRHAM experiments
using HadAM3H and with 30% and 7% for the ECHAM-
driven experiments for Middle Europe and Scandinavia,
respectively.
[18] RCM output is not available for the entire period
1961–2100 because transient RCM simulations are com-
putationally very demanding. Instead two 30-year time
slices are available; one representative for the climate in
the period 1961–1990
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf