(2011) Horsens Fjord Case. Background document for case study, 18 pp.
Refsgaard JC, Henriksen HJ (2011) Horsens case - Break out groups. Tasks for group work. 3 pp.
Lorenzoni I, Pidgeon NF (2006). Public views on climate change: European and USA perspectives. Climatic Change, 77, 73-95. DOI: 10.1007/s10584-006-9072-z
Stern PC (2000). Toward a coherent theory of environmentally significant behavior
/media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
thus covering a broad range of expertise on water-related issues.
The total group of stakeholders consisted of around 35 persons out of which 12–15 participated in any of the scenario workshops;
5 stakeholders participated in all three scenario development meetings. The group was completed by a number of representatives
from the SCENES project, notably regional coordinators and a number of experts
/media/loftslag/Kok_et_al._TFSC_published_2011.pdf
to be a very successful way of getting
participants to interact with each other right from the start and in general the
group was not a shy. At the icebreaker on Monday we also played a “bingo”
and learned more about each other, both teachers and participants, as the
consultant taught us.
The structure of the course had worked out well last year in Norrkoping so it
was kept approximately the same
/media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf
An article in Nature on the rifting event at Bárðarbunga
15.12.2014
Advanced online publication in Nature today reports research by an international team of geoscientists on the formation of the intrusive dyke which extends 45 km in the subsurface from the Bárðarbunga
/about-imo/news/nr/3038
buy a "Flybus Plus" ticket, further transportation
from BSÍ terminal in central Reykjavík to the hotel is included. Get a return ticket for smooth transportation back to the airport, the same way you came. You do not need to
book your ticket in advance. The Flybus operates for all arriving
flights, and even in case of flight delays it will wait for the passengers.To get around in ReykjavíkCity
/norsem/norsem2016/transportation/
summers, leading to melting permafrost in the northern part of Finland, resulting in
more frequent buckling of roadways, 5) increases in spring flooding and riparian flooding
and 6) coastal sea level rise and erosion (Jaroszweski, Chapman, & Petts, 2010).
Key uncertainties: 1) epistemic uncertainties- regionally down-scaled projected impacts,
road usage patterns, road safety data, cost data
/media/loftslag/Group4.pdf
receiver since 22-04-2011
SNAE Snæbýli ? Off-line due to hardware failure with the
receiver
10
Some of these stations are difficult to get back online without site visits. Consequently they
may therefore be out-of-service for extended periods. Based on an estimate of the
completeness of the GPS data-set in 2010, the uptime of the network is about 70.5%. For
further details, see section 6
/media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
ORIGINAL ARTICLE
Climate change adaptation in European river basins
Patrick Huntjens • Claudia Pahl-Wostl •
John Grin
Received: 1 July 2008 / Accepted: 24 December 2009 / Published online: 2 February 2010
The Author(s) 2010. This article is published with open access at Springerlink.com
Abstract This paper contains an assessment and stan-
dardized comparative analysis of the current water man
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
207 earthquakes have been
detected in the caldera. Two earthquakes were bigger then M5,0, on 31. October at 21:32 an M5,2 earthquake was
detected and M5,3 on 2. November at 16:02. In total 27 earthquakes between M4 and 5 were detected and 8
between M3 and 4.
• The GPS station in the centre of Bardarbunga show that the subsidence of the caldera continues with similar rate as
it has done over
/media/jar/Factsheet_Bardarbunga_20141103.pdf