Eins og sjá má af meðfylgjandi korti er ísinn næst landi um 77 sjml
NNV af Straumnesi, 82 sjml NV af Horni, og 146 sjml N af Skaga. Ekki var unnt að greina
ísinn vel sökum lágskýja, en útbreiðsla sést vel á SLAR myndum, sem og á eftirlitsratsjá.
Ísdreifar voru að sjá á ratsjá um 1-2 sjómílur frá megin ísröndinni.
Gunnar Örn Arnarson
Yfirstýrimaður TF-SIF
/media/hafis/skyrslur_lhg/hafisskyrsla_11052011.pdf
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 53 Impact map for airports in case of an eruption like 1362 at Öræfajökull ................ 82
Figure 54 Impact map for power lines in case of an eruption like 1362 at Öræfajökull ......... 83
Figure 55 5% PM10 probability map for an eruption like 1362 at Öræfajökull. ...................... 84
Figure 56 25% PM10 probability map for an eruption like 1362 at Öræfajökull
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
on the
Reykjanes Peninsula (boxes B-F). .................................................................... 81
Table A.3. Fault parameters for mapped fault segments and clusters in the Hengill
area and the South Iceland seismic zone (boxes G-I). ..................................... 82
Table A.4. Fault parameters for mapped fault segments on the Hestvatn fault (J-21)
(box N
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf