Projects
involving sh
Concise info
Executive
summaries
Downloadable
"Stakeholder
friendly" info
Stakeholder Relevance of the CES Project
Jenny Gode, 31 May 2010
Research programme
"Translators"
F
act
sheets
W
eb
page
Stee
ring
co
m
m
ittee
Visits
W
o
rkshops
R
efe
re
nce
g
ro
up
s
E
x
.
su
m
m
a
rie
s
M
eetings
Stakeholders
Energy companies
Energy authorities
Decision makers
Other stakeholders
/media/ces/Gode_Jenny_CES_2010.pdf
of
earthquakes.
Reference:
[1] Korja, A. and Kosonen, E. M. (eds.) 2015. Seismotectonic framework and seismic source area models in Fennoscandia,
Northern Europe. Univ. Helsinki, Instit. Seismology, Report S-63, 284 p.
http://www.seismo.helsinki.fi/pdf/Seismotectonic_S63_Korja_Kosonen.pdf
[2] Nørbech, T., Engsager, K., Jivall, L., Knudsen, O., Koivula, H., Lidberg, M., Ollikainen, M. & Weber, M., 2008
/media/norsem/norsem_korja.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
to get highly
accurate results in photogrammetric processing of historical photographs.
REFERENCE
Jóhannesson, T., H. Björnsson, F. Pálsson, O. Sigurðsson and Þ. Þorsteinsson. 2011. Lidar
mapping of the Snæfellsjökull ice cap, western Iceland, Jökull, 61,19–32.
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
12 Csatho and others
The ICESat-2 mission: design
/media/vatnafar/joklar/Reykholt-abstracts.pdf
et al., 2013). Based on satellite altimetry, the trend in absolute sea
level in the North Sea was about 1-3 mm/yr in 1992-2014, depending on location (EEA, 2017).
In the Baltic, the mean sea level rose 1.5 mm/yr in the 20th century (Nerheim et al., 2017). The
absolute sea level rise for the Scandinavian coast of the Baltic in period 1891-1990 was found to
be 1.8 mm/yr (O. Vestøl, 2006). In 1992
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
elevation
complete for Scandinavia
Icelandic Inventory (data from O. Sigurdsson)
Data
Climate data, calibration period
Monthly air temperature: ERA-40 reanalysis (0.5°×0.5°), 1958-2001
Monthly precipitation: Precipitation climatology VASClimO,
1951-2000, 0.5°×0.5° (Beck et al., 2005)
Elevation-dependent mass balance data for individual glaciers
Mass-balance data
Future projections
Glacier
/media/ces/Hock_Regine_CES_2010rs.pdf
will develop. However, four scenarios
are considered most likely:
o The migration of magma could stop, resulting in a gradual reduction in seismic
activity and no further eruptions.
o The dike could reach the Earth's surface north of Dyngjujökull causing another
eruption, possibly on a new fissure. Such an eruption could include lava flow
and (or) explosive activity.
o The intrusion reaches
/media/jar/Bardarbunga-2014_August-events.pdf
the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits
were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes
evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob-
servations
/media/ces/GA_2009_91A_4_Andreassen.pdf
Elvehøy, H., Guðmundsson, S., Hock, R., Machguth, H., Melvold, K., Pálsson, F., Radic, V.,
Sigurðsson, O. and Þorsteinsson, Þ.
The impact of climate change on glaciers and glacial runoff in the Nordic countries .......................................... 38
Radic, V. and Hock, R.
Volume changes of the glaciers in Scandinavia and Iceland in the 21st century
/media/ces/ces-oslo2010_proceedings.pdf
-2B. Mon. Wea. Rev., 132, 2184–
2203.
Dickinson, R. E., Errico R. M., Giorgi F. and Bates G. T. 1989. A regional cli-
mate model for the western United States. Clim. Change, 15, 383–422.
Giorgi, F. 1990. On the simulation of regional climate using a limited area
model nested in a general circulation model. J. Climate, 3, 941–963.
Giorgi, F., and Mearns L. O. 1999. Introduction to special section
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf