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NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
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1
Outline for the case Road maintenance in a changing climate
Introduction
Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and
Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
............................................................................... 20
Räisänen, J.
Probability distributions of monthly-to-annual mean temperature and precipitation in a changing climate ......... 22
Nikulin, G., Kjellström, E., Hansson, U., Strandberg G. and Ullerstig A.
Nordic weather extremes as simulated by the Rossby Centre Regional Climate Model: Model evaluation and
future projections
/media/ces/ces-oslo2010_proceedings.pdf
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf
opportunity evaluation
Case studies
NOE Net
SEAS-NVE
Findings of case studies
• Distribution companies generally well
equipped for climate change
– Cabling of all overhead lines well under way
– Distribution boxes in areas with increased risk of
flooding are elevated already
– Salt spray further inland is becoming an increasing
problem for substations and transformers
Cabling in Denmark
/media/ces/James-Smith_Edward_CES_2010.pdf
24 July 2010
This manuscript was handled by K.
Georgakakos, Editor-in-Chief, with the
assistance of Ercan Kahya, Associate Editor
Keywords:
Climate change
Flood
Hydrological modelling
Flood inundation area
Hydraulic modelling
Finland
s u m m a r y
This paper provides a general overview of changes in flooding caused by climate change in Finland for the
periods 2010–2039 and 2070–2099. Changes
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
(DGPS) equipment
in 2001. Continuous profiles, approximately 1 km apart,
were measured in the accumulation zone and a dense net-
work of point measurements were carried out in the abla-
tion zone. Digital Elevation Models (DEMs) of the surface
and bedrock were created from these data (Fig. 2; Björns-
son and Pálsson, 2004). The estimated errors are at most
1–5 m (bias less than 1 m) for the surface
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
7
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ea
n
d
is
ch
ar
g
e
(m
3 /
s)
Present: Mean A2: Mean
Station 280001: Upstream Bygholm Lake
0
5
10
15
20
25
30
35
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ax
im
u
m
d
is
ch
ar
g
e
(m
3 /
s)
Present: Max A2: Max
Station 270045: Upstream Lake Nørrestrand
0
2
4
6
8
10
12
14
16
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ea
n
d
is
ch
ar
g
e
(m
3 /
s)
Present: Max A2: Max
/media/loftslag/Horsens_case.pdf
Forsíðumynd: Svava Björk Þorláksdóttir mælir með öldustilli
niður á festur í Iðu í Hvítá. Ljósmynd: Njáll Fannar Reynisson.
V E Ð U R S T O F A Í S L A N D S / Á R S S K Ý R S L A 2 0 1 8
3
Viðburðaríkt ár er að baki
hjá starfsfólki Veðurstofunnar
enda felast jafnan margar og
fjöl breyttar áskoranir í vöktun
og rannsóknum á náttúru -
öflum landsins.
Loftslagsmál eru mjög á
döfinni enda stærsta
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf