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• Analyse future snow scenarios
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Elevation of met.no
/media/ces/Dyrrdal_Anita_CES_2010.pdf
scenario
development, with an example from Brazil
Kasper Kok *
Land Dynamics, Department of Environmental Sciences, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands
1. Introduction
The world is undergoing rapid changes while globalising
constantly, which gives the consideration of the future new
urgency and importance. Scenario development has emerged as a
key method when taking
/media/loftslag/Kok_JGEC658_2009.pdf
sides of the main debris flow paths. Point protection of individual buildings, in
particular some of the more important industrial buildings below Þófi, should also be
considered.
Contents
1 Introduction ................................................................................................ 9
2 Site description and geological setting
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
the event than in the previous eruption, but more lava is being extruded.
At 07 AM the lava flow was around 1 km wide and 3 km long towards northeast. The thickness was estimated a few meters, the flow about 1000 m3 pr second.
Approximately 500 earthquakes were detected in the area and smaller than before. The strongest earthquake, M3.8 was in the Bárðarbunga caldera. Poor weather conditions prevail
/earthquakes-and-volcanism/articles/nr/3000