or system dynamics
models, provide benets which go beyond the production of the model itself. The discussions and negotiations
between the groupmembers during themodel building, for example, improve the group’s shared understanding of the
management problem and its solutions. As such, participatory modelling can be a tool for supporting the type of social
learning currently being promoted for water
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
-
grated water management: agency, awareness raising and
education, type of governance and cooperation structures,
information management and—exchange, policy develop-
ment and—implementation, risk management, and finances
and cost recovery. This comparative analysis has an
explorative character intended to identify general patterns
in adaptive and integrated water management and to
determine its
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
Tremv-ALERT: A new early warning
system to detect volcanic tremor
Bethany Vanderhoof
Þórður Karlsson
Yesim Cubuk Sabuncu
Kristín Jónsdóttir
VÍ 2021-008
Skýrsla
Tremv-ALERT: A new early warning
system to detect volcanic tremor
VÍ 2021-008
ISSN 1670- 8261
Skýrsla
+ 354 522 60 00
vedur @vedur . is
Veður st of a Íslands
Búst aðaveg ur 7 – 9
108 Reyk j avík
Bethany Vanderhoof
Þórður Karlsson
Yesim
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
• Methodology
• Key findings
• Conclusions
2
Forestry in Finland
1. Land area distribution 2. Species distribution
Total Forestry land 26.3 mill. ha
3. Growing stocks, increment and drain 4. Site type distribution
Source: Finnish Forest Research Institute, 2008
3
Forest management
Final felling
Timber
Energy biomass
Thinning
Timber
Pre-commercial or
energy biomass thinning
Regeneration Regeneration
4
/media/ces/Alam_Ashraful_CES_2010.pdf
!
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jan feb mar apr mai jun jul aug sep okt nov des
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55550 Hafslo
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jan feb ar apr ai j j l t
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55550 Hafslo 54130 Lærdal
Ensemble approach for probabilistic
hydrological projections
Catchment
/media/ces/Lawrence_Deborah_CES_2010.pdf
indicates that about 60 million cubic metres of material are in motion. It is possible that the entire mass may be released as a single rockslide, it is also possible that the material may be released as several smaller rockslides. The age of these fractures is not well known. They are not visible on aerial imagery from the year 2003 but they are evident in an elevation model from 2011, indicating
/about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull
Type: Subglacial volcano with caldera
Summit ice cover: Yes
Dominant type of activity: Basaltic explosive, phreatomagmatic
Magma type: Basalt dominant
Known precursors: No information
Expected precursors: Significant increase in seismic activity
Monitoring level: High
Current seismicity: Seismic swarms from 16 August 2014. See http://vedur.is for live
information
Eruption
/media/jar/Bardarbunga_kafli20140825.pdf