Access, can be monitored closely on the EUROVOLC website: https://EUROVOLC.eu. The EUROVOLC project can also be
followed on social media through the dedicated #eurovolc and @eurovolc usernames on Twitter and Instagram, and Facebook. Geographical distribution of European volcanoes (red circles): on the
European continents,
plus Canary islands (left) and in overseas countries (right
/about-imo/news/eurovolc
Denmark, DK). Participatory planning processes - Group model building
10:00 p9 Simo Haanpää (Aalto University, Fi). Ilmasto-opas.fi (ClimateGuide.fi) web portal - a new tool for managing climate change in Finnish municipalities
10:30 tea/coffee break
11:00 break out sessions : Thursday cases revisited
12:00 - 13:00 lunch
13:00 p10
Helle Katrine Andersen (DANVA, Dk). DANVA CC adaptation plan
/nonam/workshop/program/
to c. 10% increase
Uncertainty related to choice of GCM
• Changing seasonality (2021-2050 vs 1961-1990)
in Sweden
T2m Precipitation Wind speed
Colored lines represent averages over RCMs forced by the same GCM
Gray field is max/min of all RCM simulations
An example of CC in the next few decades
2011-2040
vs
1961-1990
Why are differences between ensemble
members so large?
Winter (DJF)
M
S
L
P
T
2
/media/ces/Kjellstrom_Erik_CES_2010.pdf
plumes are seen somewhat lower and mark the front of the lava stream. The size of the eruptive crater is 280 x 190 m. Lava splashes are thrown at least a few hundred meters into the air.
Overall assessment is that it is more explosive activity and ash production than was observed yesterday. Progression of the lava seems to be slower than yesterday.
Presently there are no indications
/earthquakes-and-volcanism/articles/nr/1884
Holuhraun lava field
Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather and visibility, shows the outlines of the new lava in exceptionally high detail (see full image) as they were two days ago. Referral: (c) DLR/ Fjarkönnun ehf./IsViews 10/2014.
9 October
/earthquakes-and-volcanism/articles/nr/3011
the following five parameters
were adjusted: (1) Storage coefficient of direct runoff kd; (2) storage coefficient of
interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and
(5) the recession constant krec for the decreasing saturated hydraulic conductivity with
increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic
conductivity in the X/media/ces/2010_016.pdf