on the transport sector. Table 1 below shows a tentative distribution of activities
by different stakeholders and by geographic / administrative aggregation level.
Table 1 – Tentative identification of relevant (predominant) operating levels and actors
Local Regional National* International
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for
some work to be done on Tuesday evening 28 August.
Short presentations of own dissertation study
All 13 participating PhD students are requested to give an 7 minutes presentation about their own
dissertation study. This is done in two batches on Monday and Tuesday morning respectively.
Lectures
The three scheduled lectures concern topics which scored high among the indicated topics in the PhD
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
initiation and adoption. Quality of research
results.
7. How to assess when to enter a learning cycle and how to assess outcomes and progress?
How to assess the appropriate level of sophistication and complexity of decision process and
methods? How to integrate adaptation solutions and how to evaluate outcomes of learning
cycles?
With reference to the introductory presentation (see section 2/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
-473.
Gabriel, D., S. M. Sait, J. A. Hodgson, U. Schmutz,
W. E. Kunin, and T. G. Benton. 2010. Scale matters:
the impact of organic farming on biodiversity at
different spatial scales. Ecology Letters 13
(7):858-869.
Gibson, C. C., E. Ostrom, and T. K. Ahn. 2000. The
concept of scale and the human dimensions of global
change: a survey. Ecological Economics 32:217-239.
Hare, M., and P. Deadman
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Spatial perception of flood hazard in the urban area of Selfoss
Emmanuel P. Pagneux 1, 2
1 Icelandic Meteorological Office
Grensásvegur 9 – 108 Reykjavík – ICELAND
2 Department of Geography and Tourism
Faculty of Life and Environmental Sciences / School of Engineering and Sciences
University of Iceland
Aska, Sturlugata 7 – 101 Reykjavík – ICELAND
Email: emmanuel@vedur.is
/media/loftslag/Spatial_perception_of_flood_hazard_in_the_urban_area_of_Selfoss,_Iceland.pdf
scenario Summer Winter
Temp ▲6˚c ▲7˚c.
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CO N l d bl2 ear y ou e
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than can be expected to originate from the cauldrons, three to four times the wa-
ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has
been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be
2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich
groundwater from the glacier comes from the cauldrons
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf