Council on Water Resources, Carbondale, IL,
1998).
12. K. E. Schilling, E. Z. Stakhiv, in Global Change and Water
Resources Management (Water Resources Update No.
112, Universities Council on Water Resources,
Carbondale, IL, 1998).
13. J. R. Stedinger, D. Pei, T. A. Cohn, Water Resour. Res. 21,
665 (1985).
14. Z. W. Kundzewicz, L. Somlyódy, Water Resour. Manage.
11, 407 (1997).
15. P. C. D. Milly, K/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
Jónsdóttir et al (2022). Acoustic Signals of a Meteoroid Recorded on a Large‐N Seismic Network and Fiber‐Optic Cables. Seismological Research Letters 2022. doi.org/10.1785/0220220236
Lamb, O.D., Gestrich, J.E., Barnie, T.D., Jónsdóttir, K., Ducrocq, C., Shore, M.J., Lees, J.M., Lee, S.J (2022). Acoustic observations of lava fountain activity during the 2021
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uncertainty and investment risk in the power sector: A literature review. CICERO. 22 p.
Linnerud, Kristin (2009) How to improve the risk assessment procedure to better reflect a financial perspective to risk. CICERO. 11 p.
Jylhä, K. (2008). Some notes from the CES Risk Assessment Workshop 30-31 October 2008 in Tampere, Finland. Nordic Climate Workshop, 4-5 Nov 2008, Helsinki, Finland.
Other, Talks
/ces/publications/nr/1941
of climate change on the routine and periodic maintenance of roads. Helsinki
2009. Finnish Road Administration, Central Administration. Finnra reports 8/2009, 66 p. +
app. 8 p. ISSN 1459-1553, ISBN 978-952-221-172-9, TIEH 3201122-v. (in Finnish, abstract in English)
[5] Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P., Haapala, J., Jylhä, K., Tolonen-Kivimäki, O.,
and Tuomenvirta, H
/media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.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
ÁRSSKÝRSL A 2018
2
Á R S S K Ý R S L A 2 0 1 8
3 Frá forstjóra
4 Veðurstofan 2009–2019
12 Náttúrufar
18 Rannsóknir
20 Fjármál og rekstur
22 Ritaskrá starfsmanna
?Veðurstofa Íslands 2019
Bústaðavegi 7–9, 108 Reykjavík
ISSN 2251-5607
Efni ársskýrslunnar var unnið af starfsmönnum
Veðurstofu Íslands
Ritstjórn: Sigurlaug Gunnlaugsdóttir
Hönnun og umbrot: Hvíta húsið
Prentun: Prentmet
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
and providing early-warning mechanism information.
Figure 1. Map showing SW-Iceland, the focus area within SAFER. Seismicity during
1997–2000, defining many of the already mapped faults, is shown colour coded
according to age. Events with M>5 are shown as stars. The outline of the South Iceland
Seismic Zone (SISZ) is shown with orange dashed lines. Test sites are marked on the map
with letters K, H, Á
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
Such landslides fall from a comparatively high
elevation, cause extensive disruption and upheaval of loose materials and soils in their
way, and can travel considerable distances uphill against opposing slopes.
Secondly, there are medium-sized or large, rapid debris flows that are released from com-
paratively high elevations and are confined to gullies as they travel down the mountain-
side, similar
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf