on 26-28 August 2012 in Helsinki, directly linked to the 2nd Nordic International Climate Change Adaptation Conference, 29-31 August 2012, Helsinki (see pdf, 0.5 Mb).
Practical information
Programme for PhD workshop preceding the conference (pdf 0.53 Mb)
Guidelines for rapporteurs (pdf 0.38 Mb)
Floor plan - location of Workshop rooms (pdf 0.26 Mb)
Themes
The themes of the PhD workshop
/nonam/adaption/phd-workshop-2012/
Veðurstofa Íslands
2 Almannavarnadeild Ríkislögreglustjóra
3 Jarðvísindastofnun Háskólans
4 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Bologna
5 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Pisa
6 Jarðvísindadeild Háskóla Íslands
7 Agricultural University of Iceland
8 Consultant
Skýrsla nr. Dags. ISSN Opin Lokuð
VÍ 2020-011 Desember 2020 1670-8261 Skilmálar:
Heiti skýrslu
/media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
change. These values are not to be used for further research as they are preliminary and all rights to the data belong to the scientists who are acquiring and interpreting the data.
The participating institutions include: Icelandic Meteorological Office, Chalmers University of Technology, Istituto Nazionale di Geofisica e Vulcanologia, Düsseldorf University of Applied Sciences, University of Palermo
/earthquakes-and-volcanism/articles/nr/3001
University
of Technology, Istituto Nazionale di Geofisica e Vulcanologia, Düsseldorf University of
Applied Sciences, University of Palermo, University of Cambridge, and British Geological
Survey.
18 September 2014 11:30 - from the Scientific Advisory Board
Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences University
of Iceland along with representatives from
/media/jar/Bardarbunga-2014_September-events.pdf
change. These values are not to be used for further research as they are preliminary and all rights to the data belong to the scientists who are acquiring and interpreting the data.
The participating institutions include: Icelandic Meteorological Office, Chalmers University of Technology, Istituto Nazionale di Geofisica e Vulcanologia, Düsseldorf University of Applied Sciences, University of Palermo
/earthquakes-and-volcanism/articles/nr/3001/
- 23rd of August, when the pressure in the magma reservoir had fallen substantially. This fall in magma reservoir pressure is considered to have triggered the caldera collapse. The continuation and rate of collapse was controlled by flow path properties and the load of the caldera floor overlying the magma reservoir. As the collapse progressed the height of centre of the caldera declined
/about-imo/news/on-the-bardarbunga-gradual-caldera-collapse
- 23rd of August, when the pressure in the magma reservoir had fallen substantially. This fall in magma reservoir pressure is considered to have triggered the caldera collapse. The continuation and rate of collapse was controlled by flow path properties and the load of the caldera floor overlying the magma reservoir. As the collapse progressed the height of centre of the caldera declined
/about-imo/news/on-the-bardarbunga-gradual-caldera-collapse/
In the case
of the valley floor in Hítardalur being grey, the growing vegetation is
believed to be the cause. In the case of the source of the landslide, it
is the only part of the mountain slope which is grey. This suggests that
rapid deformation was ongoing between the two acquisitions in the area
while the surrounding slopes were stable. (Figure from Vincent Drouin,
University of Iceland
/about-imo/news/displacements-in-fagraskogarfjall-for-some-time-before-the-landslide-fell
6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
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combined with opera-
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/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
(ECT)
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Energy wood
/media/ces/Alam_Ashraful_CES_2010.pdf