and explored. The list of earthquakes updates every five minutes. Click this link to run the model:
An interactive 3D model of the earthquakes in Bárðarbunga – preliminary version
However, this is a preliminary version; the model is still being developed. There are some browser issues, e.g. Google Chrome and Firefox run it, IE10 does not; other browsers have yet to be tested. In some instances
/earthquakes-and-volcanism/articles/nr/2971/
estimated to be 11 Mt (+/- 5 Mt) for the entire duration of the eruption (Gislason et al., 2015).
SO2 can have human and animal health implications when present in high concentrations. For this reason, IMO was asked to provide hazard maps for SO2 ground concentration at local and regional scale. The maps were produced using the dispersal model CALPUFF. The maps were used to identify and draw/pollution-and-radiation/volcanic-gas/hazard-zoning/
estimated to be 11 Mt (+/- 5 Mt) for the entire duration of the eruption (Gislason et al., 2015).
SO2 can have human and animal health implications when present in high concentrations. For this reason, IMO was asked to provide hazard maps for SO2 ground concentration at local and regional scale. The maps were produced using the dispersal model CALPUFF. The maps were used to identify and draw/pollution-and-radiation/volcanic-gas/hazard-zoning
at Upptyppingar (measuring 165-210 microSiemens/cm). We cannot yet
draw conclusions about possible changes in the contribution of gases from the volcanic/geothermal
system to the hydrological system.
Conditions at eruption site
No eruption.
Seismic tremor
No sign of harmonic (volcanic) tremor detected.
Earthquakes
Intense earthquake activity continues at the Bárðarbunga volcano – a situation that has persisted
/media/jar/Bardarbunga_daily_status_report_22082014.pdf
in the multidisciplinary nature of the project which gives new insights for the project participants. Thus, the project provides a useful framework also for Nordic research education and postdoctoral researchers, contributing to enabling academia to pursue high-level expertise and a competence pool that the Nordic energy sector may draw on in the future.
Participants and organization of project
/ces/project/
upper and lower limits for
water level defined as certain water levels on specific dates. These regulation limits
often include a mandatory draw-down of water level during late winter and early
spring in order to make storage space for the snowmelt flood. The regulation permits
and limits have been developed using past observations based on an assumption of
stable hydrology (Kundzewicz et al
/media/ces/Water_resources_man_Veijalainen_etal.pdf
and experimentation, and still
have an impact on the management practice. We
draw on recent experiences gained in a participatory
process in the Dhuenn catchment, a sub-catchment
of the Wupper basin in the German Rhine basin area,
thus following a broadly bio-regional approach. The
whole participatory process can be considered as a
management experiment. It was developed to
promote the continuous
/media/loftslag/Daniell_etal-2010.pdf
July and August (JJA). The blue boxes enclose a few stations on
flat land in S-Iceland where the observations and simulations are in reasonable agreement. The
red boxes draw attention to stations in N-Iceland where the model overestimates precipitation,
despite these stations being on flat land. Stations that have huge overestimation, which is almost
certainly due to non-resolved orography
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
by the electorate.
Accordingly, public views on climate change have been of interest to many
researchers and policy makers for several years now. These have been elicited
through a range of different methods, primarily quantitative social surveys and
more recently in-depth qualitative studies. In this overview of European and USA
public opinions and attitudes regarding climate change, we draw upon findings
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf