and no earthquake over M5.0 since January 8th.
Around 60 earthquakes were detected in the dyke during the same period. The strongest ones were measured M1.4
and M1.3. It is worth to mention that bad weather does affect the number of small earthquakes detected.
The rate of the subsidence in Bárðarbunga caldera last week was about 5 cm per day in light of the ice subsidence
/media/jar/Factsheet_Bardarbunga_20150227.pdf
University of Iceland along with
representatives from the Icelandic Civil Protection, the Environmental Agency of Iceland and the Directorate of
Health.
Main points
Volcanic eruption in Holuhraun
Air quality
Scenarios
Notes
The volcanic eruption in Holuhraun continues with similar intensity.
Seismic activity in Bardarbunga continues to be strong. Since Wednesday, 5. November
/media/jar/Factsheet_Bardarbunga_20141107.pdf
(causal loop modelling) Daniel, Ferrand, Hare etal
AquaStress Project
Cognitive mapping and Group model building
• … are contrived methods
• used when it is difficult for people to explain how systems work (even when they know)
1. SH individual cognitive map
(causal loop modelling) Daniel, Ferrand, Hare etal
AquaStress Project
Cognitive mapping
a108 Elicits a cognitive map representing what
/media/loftslag/Hare_1_Part2.pdf
and uncertainty in a practical way.
The term tool (for AM) is broadly framed, which implies
that tool enhancement (for AM) can have different mean-
ings. Tool enhancement can guide when and how to use a
certain tool in the planning cycle in relation to IWRM or
the water framework directive (WFD). It can consist of
structuring the tool according to a transition framework to
AM e.g. from the NeWater
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
/ interaction), 4) engage / active involvement and 5) partner / co-decision
making.
3. Which knowledge is needed regarding climate effects and the involved uncertainties, and
how do we obtain such knowledge?
Knowledge is expertise, skills, what is known, facts, information and awareness or familiarity.
Uncertainty can relate to framing, emission scenario, GCM, RCM, downscaling, local
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
.............................................................................................. 45
5.3 Present weather ..................................................................................... 45
Appendix ......................................................................................................... 47
5
List of Figures
1 How PWD22 determines the type of precipitation. ........................................ 11
2 Number of records as a function of the height
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens
fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and
scattered habitation. One of the most important plant community on the islands are along the East coast
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens
fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and
scattered habitation. One of the most important plant community on the islands are along the East coast
/media/loftslag/Case_A___Horsens_Fjord.pdf
in the
preceding review sessions. The messages can be requests, critical questions, propositions for emphasis on
certain topics in future research and/or implementation, educational wishes, etc. In the opening plenary
session of the Adaptation Conference on Wednesday morning two PhD students (one from each group) will
present the messages (max. 5 minutes each).
2
Tasks in the Conference
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
in Seyðisfjörður
VÍ 2016-006
ISSN 1670-8261
Report
+354 522 60 00
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
108 Reykjavík
Daniel Illmer, Ingenieurbüro Illmer Daniel e.U.
Jón Kristinn Helgason, Icelandic Met Office
Tómas Jóhannesson, Icelandic Met Office
Eiríkur Gíslason, Icelandic Met Office
Sigurjón Hauksson, Efla Consulting Engineers
5
Abstract
Evaluation and interpretation
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf