). NeWater is based on the
hypothesis that IWRM cannot be realised unless current
management regimes undergo a transition towards more
0301-4797/$ - see front matter r 2007 Elsevier Ltd. All rights reserved.
doi:10.1016/j.jenvman.2007.05.009
Corresponding author. Tel.: +45 38 14 27 71; fax: +45 38 14 20 50.
E-mail address: hjh@geus.dk (H.J. Henriksen).
(Downing et al., 2005). Vulnerability
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-year return period, based on the complete ICRA dataset. Timeseries were
extracted using the average value of all the grid-points within the catchment. 1M5 value
is shown in red.
Hálslón
2 years 5 years 10 years 25 years 50 years 100 years
3 hours 8 11 13 15 18 20
6 hours 18 23 27 31 36 39
12 hours 35 43 49 54 62 67
24 hours 60 70 78 85 94 101
48 hours 91 105 115 125 137 147
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they started recording and the highest recorded values. ...................................... 24
Table 2. Evaluation of the four interpolation methods for scatter and Q–Q plots. ................... 31
Table 3. The values and dates of the 20 highest daily values of precipitation in Neskaupstaður
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the
tendencies already observed, while their magnitudes as well as interscenario differences are
increasing towards the end of the 21st century.
Table 1
Model, country Resolution
atmosphere/ocean
1 CGCM3.1(T47), Canada T47L31/1.9°×1.9°L29
2 CNRM-CM3, France T63L45/0.5-2°×2°L31
3 CSIRO-Mk3.0, Australia T63L18/0.8°×1.9°L31
4 ECHAM5/MPI-OM, Germany T63L31/1.5°×1.5°L40
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(2011) Horsens Fjord Case. Background document for case study, 18 pp.
Refsgaard JC, Henriksen HJ (2011) Horsens case - Break out groups. Tasks for group work. 3 pp.
Lorenzoni I, Pidgeon NF (2006). Public views on climate change: European and USA perspectives. Climatic Change, 77, 73-95. DOI: 10.1007/s10584-006-9072-z
Stern PC (2000). Toward a coherent theory of environmentally significant behavior
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