less than
10/10
9+
10/10 10
Undetermined or unknown x
Concentration (C)
C – Total concentration of ice in the area, reported in tenths (see symbols in table 3.1).
Note: Ranges of concentration may be reported.
Ca Cb Cc – Partial concentrations of thickest (Ca), second thickest (Cb) and third thickest (Cc)
ice, in tenths.
Note: Less than 1/10 is not reported. 10/10 of one stage of development
/media/hafis/frodleikur/ice-chart_colour-code-standard.pdf
Denmark, DK). Participatory planning processes - Group model building
10:00 p9 Simo Haanpää (Aalto University, Fi). Ilmasto-opas.fi (ClimateGuide.fi) web portal - a new tool for managing climate change in Finnish municipalities
10:30 tea/coffee break
11:00 break out sessions : Thursday cases revisited
12:00 - 13:00 lunch
13:00 p10
Helle Katrine Andersen (DANVA, Dk). DANVA CC adaptation plan
/nonam/workshop/program/
to c. 10% increase
Uncertainty related to choice of GCM
• Changing seasonality (2021-2050 vs 1961-1990)
in Sweden
T2m Precipitation Wind speed
Colored lines represent averages over RCMs forced by the same GCM
Gray field is max/min of all RCM simulations
An example of CC in the next few decades
2011-2040
vs
1961-1990
Why are differences between ensemble
members so large?
Winter (DJF)
M
S
L
P
T
2
/media/ces/Kjellstrom_Erik_CES_2010.pdf
Figure 8. Stations ranked according to their average CC for the 20 highest rainfall daily events.
................................................................................................................................................... 33
Figure 9. Ranked values of the 50 highest 24-hour accumulated precipitation events plotted
against ranked values of the 50 highest daily precipitation
/media/vedurstofan-utgafa-2020/VI_2020_008.pdf
and people are encouraged to view their
web pages, twitter streams and Facebook pages.The volcanic eruption in Geldingadalir has now been ongoing for nine days. The
lava is basaltic and highly fluid with little explosive activity. It is a very
small eruption and the lava flow has been steady at 5-7 m3/s since its onset.
Currently the extent of the lava field is within Geldingadalur
/about-imo/news/earthquake-swarm-in-reykjanes-peninsula
as river discharge and
water levels. Notices on avalanches and sea-ice
are shown; short articles and news are presented.
Furthermore, web and data portals can be accessed
through the web, which is available in both Icelandic
and English. IMO uses the social networking website
Facebook for communication and feed-back. A new
web-application (App) provides access to forecasts
and warnings
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
et
al
.(
200
4)
21
.Explici
tconsideratio
n
o
funcertaint
y
(relate
dt
o
CC
impacts
)
Uncertaintie
s
ar
e
no
t
glosse
d
ove
r
bu
tcommunicate
d
(in
fina
lreports
,orally
)
Diet
z
et
al
.(
200
3),
Brugnac
h
et
al
.(
200
8)
Researcher
s
ar
e
willin
g
to
tal
k
wit
h
stakeholder
s
abou
tuncertaintie
s
Diet
z
et
al
.(
200
3),
Brugnac
h
et
al
.(
200
8)
22
.Broa
d
communicatio
n
(on
CC
impacts
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
erations
which will be
done to protect
against th e
phenome na a nd
its
conse quenc es
The
consequenc es
of the
phenom ena to
the distribution
network
T he
con seque nc
es of the
phe nom ena
to the
pow er
plant
The conse quence s
of the phe nomena
to e nerg y sourc e
and its usability
Probability
according
to IP CC
2007
Phe nom ena acco rding
to regional scena rio
/media/ces/Keranen_Jaana_CES_2010.pdf