declaredby the Scientific Board
Location map (detailed)around the new lava field
Bárðarbunga earthquakes3D interactive model
Thickness and volumeestimate from January 1st
Comparing historic sizes of lavafields: AD 934 and 1783
Gas dispersion model
Preliminary flood risk assessmentfor Jökulsá á Fjöllum
Web cameras of Míla
Web cameras of M&T
/earthquakes-and-volcanism/articles/nr/2040
Department of Geography and Economic History, Umeå University, Umeå 90187, Sweden.
Tel. +46-90-786 50 80. Fax. +46-90-786 63 59
Abstract
A coherent application of a multi-level framework that takes interactions between levels and
how these are shaped by the political system into account is a prerequisite for understanding
the development and implementation of climate change adaptation policies
/media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf
This bridge has since been replaced
with a shorter one. Climate projections indicate that the thinning
and retreat of Icelandic glaciers and ice caps is set to continue, by the end
of the 21st century Langjökull ice cap is expected to have lost ~85%
of its volume in the warmest scenario considered, and in the same scenario
Hofsjökull and the southern part of Vatnajökull ice caps lose ~60
/climatology/iceland/climate-report
This bridge has since been replaced
with a shorter one. Climate projections indicate that the thinning
and retreat of Icelandic glaciers and ice caps is set to continue, by the end
of the 21st century Langjökull ice cap is expected to have lost ~85%
of its volume in the warmest scenario considered, and in the same scenario
Hofsjökull and the southern part of Vatnajökull ice caps lose ~60
/climatology/iceland/climate-report/