20
0
60
0
J F M A M J J A S O N D
0
20
0
60
0
J F M A M J J A S O N D
0
50
10
0
15
0
J F M A M J J A S O N D
0
50
10
0
15
0
J F M A M J J A S O N D
0
10
0
20
0
30
0
J F M A M J J A S O N D
0
10
0
20
0
30
0
J F M A M J J A S O N D
0
40
0
80
0
120
0
J F M A M J J A S O N D
0
40
0
80
0
120
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J F M A M J J A S O N D
0
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J F M A M J J A S O N D
0
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J F M A M J J A S O N D/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
Nesjum
0-5 5-10 10 15 20-15
2008-2018
1979-1989
Dæmi um ólíkt rennslismynstur.
100
9080
70
60
50
40
30
20
10
0
Júní
mánaðarmeðaltal
Ársmeðaltal
Rennsli
m
3 /s
Sigurvegarinn í getraun Veðurstofunnar á Vísindavöku Rannís hlaut
heimsókn á Veðurstofuna að launum. Salka Elín Sæþórsdóttir ásamt
vinum sínum, Ými og Bjarti. Með þeim á myndinni er Ragnar Heiðar
Þrastarson, fagstjóri landfræðilegra
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
occurring during
winter from 86% in the present climate to 98% in the year
2100. High evapotranspiration during summer was mainly
attributed to forests because forests were able to utilize most
of the increase in soil moisture storage that came from
winter recharge. For future studies Woldeamlak et al. [2007]
suggested use of transient models to study seasonal varia-
tions of the groundwater
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
11 / 12 MPI-ESM-LR REMO2009 45 / 85
13 / 14 IHCEC-EC-Earth RCA4 45 / 85
15 / 16 IHCEC-EC-Earth COSMO-CLM4-8-17 45 / 85
17 / 18 CNRM-CERFACS-CM5 RCA4 45 / 85
19 / 20 CNRM-CERFACS-CM5 COSMO-CLM4-8-17 45 / 85
11
3 Which domain, resolution, and models of the CORDEX
project should be selected for the analysis of 21st
century climate change in Iceland?
The subject of this chapter
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
magnitudes. (b) Seismic tremor amplitude in three different frequency bands. (c) Volcanic plume
height. (d) Number of lightning. Lightning and tremor amplitude roughly correlate with plume
height.
Intensifi ed human activity and a growing
population have changed the climate and the
land biosphere. One of the most widely recog-
nized human perturbations is the emission of
carbon dioxide (CO2
/media/jar/myndsafn/2005EO260001.pdf
in
Norway was provided by the Norwegian Water Resources and Energy Directorate (NVE).
TóJ 12 5.12.2009
Memo
References
Bahr, D. B., M. F. Meier and S. D. Peckham. 1997. The physical basis of glacier volume–area
scaling. J. Geophys. Res., 102(B9), 20,355–20,362.
Björnsson, H., and F. Pálsson. 2008. Icelandic glaciers. Jökull, 58, 365–386.
Fenger, J. (Ed.). 2007. Impacts of Climate Change on Renewable
/media/ces/ces-glacier-scaling-memo2009-01.pdf
separately for each calendar month at
four grid points, are depicted in Fig. 5. There are a number of cases in which the proba-
bility of the change exceeds 75% or even 90%. Among these, the decline of insolation in
eastern Finland (Fig. 5(d)) in April and November appears to have the highest probability.
Fig. 5. Monthly probability distributions for the percentage change of incident solar radiation from
/media/ces/CES_D2.4_solar_CMIP3.pdf
Av. Ed.
Belin, 31400 Toulouse, France
Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011
Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011
Abstract. The Little Ice Age maximum extent of glaciers in
Iceland was reached about 1890 AD and most glaciers in the
country have retreated during the 20th century. A model for
the surface mass balance
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf