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line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm at Bárðarbunga on Saturday
/earthquakes-and-volcanism/articles/nr/3000/
in the data used in making the
decision and the factors are interlinked, all of which makes
the problem highly complex. The part of the net defined by
variables and links is relatively easily communicated to
stakeholders (Henriksen et al., 2007b). However the
tal Management 88 (2008) 1025–1036
quantitative part, with the conditional probability tables
(CPTs), the numbers, is the step where
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
Road transport
operation and
infrastructure planning
– case Finland
Heikki Tuomenvirta and Adriaan Perrels
Climate Change Research Unit
Socie-economic impacts of climate and weather
+ ca. 5000 (streets, private, etc)
VENÄLÄINEN, A. and KANGAS, M., 2003. Estimation of winter road maintenance costs using climate data. Meteorol. Appl. 10, 69-73.
INCREASE OF TRAFFIC VOLUME 2006 -> 2030
/media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf
grundvelli myndatöku með
flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu
flóðfara og við mat á útbreiðslu og umfangi hlaupa.
Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða
grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta
undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og
myndun gosrása staðfest af meiri nákvæmni en áður. Þó
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
Vestmannaeyjar, 12 km off the south coast of Iceland. It is surrounded by sea to the east, south and west. The elevation above sea level is 118 m. Distance from the fishing town on the island is 4.5 km, distance to the nearest village on shore is 40 km and distance to the nearest town on shore is 70 km. That town has less than 5000 inhabitants. This is an ideal seashore background station at 63°N, 20°W
/pollution-and-radiation/pollution/
is calculated to be around 5000 m3/s. This size of flood will most
likley not affect the infastructure in the area such as roads or bridges. These
forecasts are uncertain at this early stage. There are past examples of Grímsvötn eruptions starting
following a flood. The loss of the water from Grímsvötn lake reduces the
pressure on top of the volcano and this can allow an eruption to begin
/about-imo/news/icesheet-in-grimsvotn-subsiding
in five-year basis
Current state of the road network affects the possible decisions to be made at the moment
Political adaptation
Management structures have to be more flexible and ready to apply adaptive management
Technological adaptation
0
1000
2000
3000
4000
5000
6000
1985199019952000200520102015202020252030
vans (mln.
tonkm)
lorries (mln.
tonkm)
0
10000
20000
30000
/media/loftslag/Group3-Road-scenarios.pdf