efficient to carry out the rest of the
risk-management process and plan development in-
house. The researcher, surprised at this suggested
change of plans, reacted strongly against the
suggestion. She argued that such a change would be
inefficient and that it contradicted a previous
statement by the project manager that using a
participatory process would allow the participants
to do the work and make
/media/loftslag/Moellenkampetal_etal-2010.pdf
analyzes real-time data and creates an alert or warning about
volcanic tremor. The most difficult aspect of creating an efficient volcanic tremor detector is
isolating the desirable signals from unwanted, non-volcanic sources that can appear at multiple
frequency bands and trigger the warning module. For instance, a detector for volcanic tremor
should avoid triggering with storm tremor, which rises
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
and risks, on the regulatory and costs effects of explicit adaptation policy, on
the interaction with other policies (mitigation, clean air, urban zoning, safety etc), and on the
ability of the road transport sector (incl. its infrastructure and supporting services) to co-
operate coherently to find efficient and timely answers9.
3. Deliberation of key questions regarding stages in adaptation
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
metaphor suggested by Argyris (1985) which is about
uncovering what happens, reflecting and understanding.
We explain that double loop learning is when one is trying
to examine the underlying assumptions one is not normally
even aware one is making.
The water managers then suggest that BNs could be used
to say something about how efficient resources are used in
the environmental management
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
in ddfi. The likely
reason for this larger effect could be that the degree-day co-
efficient for snow affects larger area of the glacier, the ac-
cumulation area, and increasing the melt of snow raises the
equilibrium line altitude and lowers the albedo, a positive
feedback which increases the melt.
6.2 Reconstruction of the 20th century evolution
The observed 1890 glacier geometry was used
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
we calculated pre-cipitation sums, Pw, from 15 September to 14 Mayin the following year. The correlation (r) and co-
efficient of determination (r2) between winter pre-cipitation and bw were obtained for each station forthe period of mass balance measurements 1949–2006.Data from the southwestern precipitation station
Røldal showed the best correlation between Pw andmeasured bw (r=0.84) (Table 1
/media/ces/GA_2009_91A_4_Andreassen.pdf
was therefore formed
by ice lifting and deformation induced by subglacial water pressures higher than ice
overburden pressure.
The discharge data and the derived size of the subglacial flood path, as indicated
by the volume of water stored subglacially, indicates a development towards more
efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the
iii
range 80–90 m3 s 1
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf