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• become severe when they cover a large region and persist for an
extended period.
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Anne K. Fleig et al. “Regional hydrological droughts and weather types in north
/media/ces/AnneFleig_May2010_CES.pdf
?
Methodological reflections on scalar structuration.
Progress in Human Geography 25:591-614.
Bryan, B. A., N. D. Crossman, D. King, W. S.
Meyer. 2011. Landscape futures analysis: assessing
the impacts of environmental targets under
alternative spatial policy options and future
scenarios. Environmental Modelling and Software
26(1):83-91.
Buizer, M., B. Arts, and K. Kok. 2011. Governance,
scale
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
ERA-40 and six GCMs
ERA4
0 GC
M
Seasonal temperature cycles averaged over 1961-2001
ERA-40 and six GCMs
ERA4
0 GC
M
’local scaling’
Method
Step 1: Calibrating an elevation dependent mass balance model
to 44 glaciers
b(h)= - M(h) + C(h) + R(h)
hmin
hmax
ELA
Woodward et al., 1997
Melt
Snow accumulation
Refreezing
Results
Global volume projections for 21th
century
(11%)
(28
/media/ces/Hock_Regine_CES_2010rs.pdf
of Time-
Variable Gravity Show Mass Loss in Antarctica. Science,
311, 5768, 1754 – 1756. DOI: 10.1126/science.1123785.
Wouters, B., D., Chambers and E. J. O. Schrama. 2008.
GRACE observes small-scale mass loss in Greenland.
Geophys. Res. Lett., 35, L20501, doi:10.1029/2008GL034816.
Meier, F. M., and others. 2007. Glaciers Dominate Eustatic
Sea-Level Rise in the 21st Century. Science, 317,
1064–1067
/media/ces/Johannesson_Thomas_CES_2010.pdf
were collected through a mail survey in Sweden,
Acceptability of travel demand managemen
of problem awareness, persona
Louise Erikssona,b,, Jo¨rgen Garvil
aDepartment of Psychology
bTransportation Research Unit
Available onlin
Abstract
y 26 (2006) 15–26
t measures: The importance
norm, freedom, and fairness
la,b, Annika M. Nordlunda,b
a˚ University, Sweden
Umea˚ University, Sweden
14 July 2006
/media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
Overview of landslide hazard and possible
mitigation measures in the settlement
southeast of Fjarðará River in Seyðisfjörður
Daniel Illmer
Jón Kristinn Helgason
Tómas Jóhannesson
Eiríkur Gíslason
Sigurjón Hauksson
VÍ 2016-006
Report
Cover photo: Jón Kristinn Helgason, 11 September 2015
Overview of landslide hazard and possible
mitigation measures in the settlement
southeast of Fjarðará River
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
swarm in December 2019 until the beginning of the eruption (Graph:
Skjálfta-Lísa from the Icelandic Meteorological Office (IMO)). Satellite
and GPS signals showed that a magmatic dyke extended southwest from Keilir to Fagradaslfjall
(Figure 2 A&B) and was getting shallower day by day. Uncertainty remained whether
the intrusion would result in an eruption. “For
the deformation team the period
/about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months
swarm in December 2019 until the beginning of the eruption (Graph:
Skjálfta-Lísa from the Icelandic Meteorological Office (IMO)). Satellite
and GPS signals showed that a magmatic dyke extended southwest from Keilir to Fagradaslfjall
(Figure 2 A&B) and was getting shallower day by day. Uncertainty remained whether
the intrusion would result in an eruption. “For
the deformation team the period
/about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/