of events closely.
Photo: Sigurlaug Gunnlaugsdóttir.
Bárðarbunga
Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com-
munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson.
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
5
The magma intrusion from Bárðarbunga
to the eruption site at Holuhraun and
related tremor pulses
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
) and changing climate (CC:CC)
1. Current climate (CU)
- varying thinning regimes
(0%, 15%, 30%,45%)
2. Changing climate (CC)
- varying thinning regimes
(0%, 15%, 30%,45%)
3. Current (CU) &
changing climate (CC)
- current thinning regime
4. Current (CU) &
changing climate (CC)
- changed thinning regimes
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/media/ces/CES_BioFuels_Flyer_new.pdf
/EPP 2
Stakeholders analysis
26 August 2011 PM/YZ/EPP 3
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/media/loftslag/Group5-Stakeholders_involvement.pdf
at the operational/local level.
A calibrated approach (standardized questionnaires and
interviews, expert judgment, and reinterpretation of out-
comes by means of relevant literature) was used to com-
pare the state of affairs in water management in the
selected case-studies.
Adaptive and integrated water management
Given the expected increase of climate-related extreme
events, water governance capabilities
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
……………………………………………………………………………………………………………………………………………………………………
6
Figure 1. Flow chart summarizing information and decision flows of an adaptive management inspired
adaptation planning cycle for road transport (at national strategic / tactical level)
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). This can be helpful with respect to
finding a common structure in presenting as well in session reporting (for which angles
mentioned in the opening session statements of the Workshop participants can provide
checkpoints).”
Session rapporteur allocation
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r/media/loftslag/Guidelines2-for-rapporteurs.pdf
up to ~13 km height.
BY K. S. VOGFJÖRD, S. S. JAKOBSDÓTTIR,
G. B. GUDMUNDSSON, M. J. ROBERTS, K. ÁGÚSTSSON,
T. ARASON, H. GEIRSSON, S. KARLSDÓTTIR,
S. HJALTADÓTTIR, U. ÓLAFSDÓTTIR,
B. THORBJARNARDÓTTIR, T. SKAFTADÓTTIR,
E. STURKELL, E. B. JÓNASDÓTTIR, G. HAFSTEINSSON,
H. SVEINBJÖRNSSON, R. STEFÁNSSON, AND T. V. JÓNSSON
Research, 2005), which are complemented by
three continuous GPS stations
/media/jar/myndsafn/2005EO260001.pdf
-
elled using precipitation data southwest of the gla-
cier. Results from the model compared well with re-
ported mass balance values for the period 1949–
2006, obtained correlations (r) for bw and bs varied
between 0.83 and 0.87 depending on model set up.
Reconstruction of the mass balance series for the
period 1924/1925–1948/1949 suggested a cumula-
tive mass deficit of c. 30 m w.e. mainly due
/media/ces/GA_2009_91A_4_Andreassen.pdf
example
can be given by the low cost still flood risk adaptation by implementing early warning system. But
there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens.
Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011)
2 / 3
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/media/loftslag/Group-1_Scenarios-for-AWM.pdf