with
three climatic scenarios
EMPS-model
Water-values and simulation
Climatic scenarios
Reference, Echam, Hadam
Data provided by NVE, SMHI and SYKE
Electricity system model in 2020
Predictions made by Eurelectric and Statnett
Fuel costs in 2020
Data provided by EA energy analyses
Sintef Energy Research Quantitative system analysis 4 of 21
Introduction
Electricity system model
Simulation results
Summary
/media/ces/Mo_Birger_CES_2010.pdf
(alb: AWS)
MODELLING LONG-TERM SUMMER AND WINTER BALANCES
? The authors 2009
Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241
ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature
/media/ces/GA_2009_91A_4_Andreassen.pdf
of market organisation alternatives
26.8.2011Adriaan Perrels/IL 10
Cost-benefit analysis – the basics 3
Simple example: despite positive IRR still cash flow challenge years 1 - 8
CBA example - initial investment 100; interest and discount 5%;
operational cost +5%/y; benefits +10%/y; IRR = 7.4%
-20
-10
0
10
20
30
40
50
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15
years
m
o
n
e
y
u
n
it
s
writing off
finance
/media/loftslag/Perrels-CBA.pdf
(Quante and Colijn, 2016). Work on risk analysis and adaptation is in different
stages in the countries of the world.
Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do
so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the
probability of such events can rise with climate change (Almannavarnir, 2011
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
bodies of management,
decision-support, risk, and participation literature.
d’Aquino (2008)
Patrick d’Aquino relies on 20 years of
implementation and evaluation experience, mostly
in a natural resource management context and in
developing countries. His approach is, at this point,
the least conceptually developed design method of
the guides presented here, although it is linked to a
theoretical
/media/loftslag/vonKorff_etal-2010.pdf
varð mest 123 m3 s 1 en rennsli hlaupsins við jökuljaðar varð mest 97 m3 s 1. Þetta
hlaup er ekki hægt að skýra með viðteknum kenningum um jökulhlaup fremur en
önnur Skaftárhlaup. Heildarrúmmál hlaupsins var 53 Gl. Geymsla vatns í hlaupfar-
veginum undir jöklinum var reiknuð út frá rennslisgögnunum en hún varð mest 35 Gl,
sem samsvarar tveimur þriðju af heildarrúmmáli hlaupsins. Geymslan í
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
the Fljótsdalsheiði region . . . . . . . 47
18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48
19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49
20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50
21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51
22 Seasonal mean
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
on the European level [e.g.
Water Framework Directive (Directive 2000/60/EC),
Common Agricultural Policy, etcetera], except for the
Ukrainian part of the Tisza. However, the Ukraine shows
strong incentives to enter the EU community and thus the
EU acquis communautaire is used as key reference for the
development of its water management principles. It was
nevertheless decided to select two case-studies
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
On the northern side a tephra wall rises 20 meters above the water. The ice walls at the southwestern corner of the crater are melting, i.e. at the site of the vent that was active 4 - 6 June. The rate of melting is assumed to be about one cubic meter per second.
Details on the volume of the lake, and possible flooding from it, in a status report issued collectively by the Icelandic Meteorological
/earthquakes-and-volcanism/articles/nr/1884