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estimates are required at locations where
streamflow series are very short or where no data are available, making a direct estimation im-
possible. Regional flood frequency analysis such as the index flood method (IFM) (Dalrymple,
1960) offers a solution to this problem. The idea is to trade space for time and compensate for
the lack of information at the site of interest by using flood data from other
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
of Iceland (Háskóli Íslands; UI) in the context of Work Package 2 of the project “Im-
proved Forecast of Wind, Waves and Icing” (IceWind), funded primarily by the Nordic Top-level
Research Initiative (Toppforskningsinitiativet; TFI), including national and private organisations.
This report is the fifth in a series of IMO reports produced for IceWind, the others being Nawri
et al. (2012d,a,b,c
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
/lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13
April 2009.
[2] WTO, World Tourism Organization (2008): “Climate Change and Tourism -
Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain.
Available at:
http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7
March 2010.
[3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for
sustainable
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.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
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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
Such landslides fall from a comparatively high
elevation, cause extensive disruption and upheaval of loose materials and soils in their
way, and can travel considerable distances uphill against opposing slopes.
Secondly, there are medium-sized or large, rapid debris flows that are released from com-
paratively high elevations and are confined to gullies as they travel down the mountain-
side, similar
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/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf