and the groundwater module. The coupling
between both modules was done by a net boundary flux between the unsaturated zone and
the groundwater (Schulla & Jasper, 2007).
Information on land use, soil type, elevation and other general properties of the watershed
are given in static distributed grids while a number of parameters describing specific
processes are adjusted to the properties of each
/media/ces/2010_016.pdf
Forsíðumynd: Svava Björk Þorláksdóttir mælir með öldustilli
niður á festur í Iðu í Hvítá. Ljósmynd: Njáll Fannar Reynisson.
V E Ð U R S T O F A Í S L A N D S / Á R S S K Ý R S L A 2 0 1 8
3
Viðburðaríkt ár er að baki
hjá starfsfólki Veðurstofunnar
enda felast jafnan margar og
fjöl breyttar áskoranir í vöktun
og rannsóknum á náttúru -
öflum landsins.
Loftslagsmál eru mjög á
döfinni enda stærsta
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
Refsgaard a,*, Jeroen P. v
Peter A. Vanroll
a Geological Survey of Denmark and Greenlan
b Copernicus Institute for Sustainable Development and Innovation
Utrecht University, Utrecht
c
Environmental Modelling & Softwar
equitable manner without compromising the sustainability of
* Corresponding author. Tel.: þ45 38 142 776; fax: þ45 38 142 050.
E-mail address: jcr@geus.dk (J.C. Refsgaard).
1364-8152
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
/EPP 2
Stakeholders analysis
26 August 2011 PM/YZ/EPP 3
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/media/loftslag/Group5-Stakeholders_involvement.pdf
of Kópasker
1.329.04 22:57:07Check.1.6 km E of Eldey
0.229.04 22:17:11Check.3.8 km ESE of Hvannadalshnjúkur
0.529.04 21:53:29Check.3.7 km NNW of Krýsuvík
0.429.04 21:44:27Check.2.5 km ENE of Krýsuvík
0.129.04 21:34:26Check.1.7 km NNE of Krýsuvík
0.429.04 21:33:14Check.1.7 km NNE of Krýsuvík
0.729.04 21:28:25Check.1.9 km WNW of Krýsuvík
0.129.04 21:22
/m/earthquakes/latest
mean surface air temperature anomalies ....................................... 28
14 Surface air temperature anomalies over Scandinavia ...................................... 29
15 Composite mean precipitation anomalies..................................................... 30
6
1 Introduction
Extratropical low-pressure systems, persisting for at least a few days, have long been recognised
as one
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf