A. Dunne, A. V. Vecchia, Nature 438,
347 (2005).
16. J. C. Knox, Quatern. Sci. Rev. 19, 439 (2000).
17. P. C. D. Milly, R. T. Wetherald, K. A. Dunne, T. L. Delworth,
Nature 415, 514 (2002).
18. Z. W. Kundzewicz et al., Hydrol. Sci. J. 50, 797 (2005).
19. R. Seager et al., Science 316, 1181 (2007).
20. IPCC, in Climate Change 2007: Mitigation of Climate
Change, Contribution of WG3 to AR4, B
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
l
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5 10 15 20
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method
De
g.
C
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ME T2m − Analysis
l vhm10
vhm19
vhm26
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vhm66
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method
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l vhm10
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Figure 3. Results of intercomparison of twenty different analogue methods. Mean error (left)
and RMSE
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
)
Best case (1.5 C increase; 2%
increase in prec)
BAU A B
Change +30 % C D
Scenario
combination
Impact
Adaptation measures
North South North South
A *
CC: Possible increase in the
amount of snow more
snow clearing increase in
operational costs
S-E: increase in traffic
volume increased wear of
roads increase in
maintenance cost.
**
CC: Possibly less snow,
more rain
/media/loftslag/Group3-The-future-of-the-Finnish-national-road-network.pdf
technologies are
being implemented which will provide a platform for a possible future ICS-D (distributed components
of the Integrated Core Services) for EPOS.
Planning and site selection process for the new instrument installations are well underway as well as
the procurement of the required equipment. In total 17 new seismological and geodetic stations will be
co-located in selected sites in Northern
/media/norsem/norsem_atakan_norway.pdf
? – D Wheeler
Simulations of the impact of Arctic sea ice on the atmospheric circulation: the need for coupled
models – D Smith
Greenland Blocking and North Atlantic Oscillation changes – E Hanna / J Overland
Group Discussion
12:45 – 14:00 Lunch (after which we move into the matsalur - lunch hall)
14:00 – 15:40
14:00 – 14:20
14:20 – 14:40
14:40 – 15:00
15:00 – 15:20
15:20 – 15:40
/media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf
distribution of runoff under present and
future conditions, Plavinas HPP
0.0
200.0
400.0
600.0
800.0
1000.0
1200.0
1400.0
1600.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
D
i
s
c
h
a
r
g
e
m
3
/
s
Observed 1961-90
SMHI-RCA3-BMC A1B 2021-50
DMI-HIRLAM-ECHAM5 A1B 2021-50
MetNo-HIRLAM-HadCM3 A1B 2021-50
Observed and modeled runoff , Plavinas
0.00
200.00
400.00
600.00
800.00
1000.00
1200.00
/media/ces/Kurpniece_Liga_CES_2010.pdf
Based on a report by
Verta et al. (2007)
92.
5
93.
0
93.
5
94.
0
94.
5
95.
0
M A MJ F J J A S O N D
Mean 19702000
Min and max 1970–2000,
natural rating curve
Target water level zone 1
Target water level zone 2
Q=+20%
Q=+10%
Q= 0%
Q=15%
Q=30%
92.90 m snow target 1
92.70 m snow target 2
Water level (m
)
Month
the regulation limits Lake Syväri has target water level zones, which are not legally
/media/ces/Water_resources_man_Veijalainen_etal.pdf
IMO in figures
? Over 600 stations in operation
? 5 offices, including the headquarters in Reykjavik
? 136 sta?and 91 additional surveillants
? Employment cost is 63% of total cost
? 65% of sta?are male
? 41% of administrators are female
? 43% of IMO income are grants
? 64% of non-governmental income is due to international projects
I C E L A N D I C M E T O F F I C E / A N N U A L R
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
Journal of Environmental Management 88
Heid
, Øste
d
e
A broad range of tools are available for integrated water resource management (IWRM). In the EU research project NeWater, a
Human dependence on water leaves us vulnerable to
climate change, flood and drought hazards, and poverty
dynamic element of vulnerable groups and their relation-
ship to water resources, and to represent the decisions
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf