/EPP 2
Stakeholders analysis
26 August 2011 PM/YZ/EPP 3
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/media/loftslag/Group5-Stakeholders_involvement.pdf
10. Rake distribution for mapped faults/clusters in box J, Hella. ........................ 97
Figure B.11. Rake distribution for mapped faults/clusters in box K, Hraungerði. ............. 97
Figure B.12. Rake distribution for mapped faults/clusters in box L, Skeið. ........................ 98
Figure B.13. Rake distribution for mapped faults/clusters in box M, Land. ....................... 98
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
presentations of own poster (2 minutes per
student) + poster session + refreshments +
formation of groups
Students
Tuesday, August 23
9:00 - 9:45 Introduction to Horsens case study on water HJH Horsens case + TOR
9:45 - 10:30 Introduction to Finnish case study on roads AP
Coffee
11:00 - 12:45 Exersize works Students
Lunch
13:45 - 15:30 Uncertainty concepts and tools JCR Refsgaard et al. (2007)
van der
/media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
and Implementation of Seismic Early Warning Processes in South-West Iceland
Kristín S. Vogfjörd, Einar Kjartansson, Ragnar Slunga, Páll Halldórsson, Sigurlaug Hjaltadóttir, Gunnar B. Gudmundsson o.fl.
83 bls.
3,2 Mb
2010-003
Use of relatively located microearthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir
104
/earthquakes-and-volcanism/reports-and-publications/
distribution of anthropogenic climate changes, largely following Räisänen and
Ruokolainen (2008a,b). The main features of this procedure are as follows:
x Model simulations of 20th and 21st century climate change are used to develop linear
regression equations that relate the local temperature or precipitation climate to a
smoothed (11-year running mean) evolution of the global mean
/media/ces/CES_D2.4_task1.pdf
increased annual runoff by 11% and 59%,
respectively, while climate change impacts resulted in an
increase in annual runoff of 26%. Loukas et al. [2002]
included altitudinal shifts in vegetation due to higher
temperatures, changes in tree cover, density, and plant
physiology in the simulations of future climate change for
two catchments in British Columbia, Canada. Average
annual actual
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
at 67 sites: (a) 100-year floods with the Gumbel
distribution and (b) average discharge.
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40
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20
Scenario number
Change in 100a Flood (%
)
Fig. 5. Box plot (median, 25 and 75 percentiles, average [diamond], max and min) of changes in 100-year floods in 2070–2099 at the 67 sites with different scenarios.
Numbering of the scenarios
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
weather stations and manual observations
Ingibjörg Jóhannesdóttir51
1,0
2019-003
Hekla volcano monitoring project. Report to ICAO
Sara Barsotti, Michelle M. Parks, Melissa A. Pfeffer, Matthew J. Roberts, Benedikt G. Ófeigsson, Gunnar B. Guðmundsson, Kristín Jónsdóttir, Kristín S. Vogfjörð, Ingvar Kristinsson, Bergur H. Bergsson, Ragnar H. Þrastarson57
4,9
/about-imo/publications/2019/
compared with current
thinning regime, increased thinning thresholds
enhanced carbon stocks in Finland under current and
changing climate. This also enhanced timber
production during 2040-2069 (2nd period) and energy
wood production at final felling during 2040-2069
and 2070-2099 (3rd period).
Results
Contact info
The ecosystem model - Sima (Kellomäki et al., 1992a,
b; Kolström, 1998) was used
/media/ces/CES_BioFuels_Flyer_new.pdf