in crops yield (Porter and Semenov 2005; Kristensen et al. 2011) and to increased risk of
nitrate leaching (Fig. 4). It is also likely that the increasing temperatures, in particular
winter temperatures, will lead to increased risks of attack by pests and diseases (Olesen et
al. 2011).
Mitig Adapt Strateg Glob Change
Tabl
e
2
Ex
am
pl
es
o
fw
at
er
re
la
te
d
cl
im
at
e
ch
an
ge
ad
ap
tat
io
n
iss
ue
/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.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/
first separately before immersing it to the DTM
of the surrounding areas. The compiled geometry data was con-
verted to grid form with a resolution of 10 m.
The hydraulic model was calibrated in each study site by adjust-
ing the Manning’s n values of bed roughness and matching the
modelled water levels with the observed ones. The observed water
level and discharge data was from the national databases
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf