for scenario runs compared with the period 1961–
1990 (shown in blue) and the more recent period 2000–2009 (shown in red) for Sandá í
Þistilfirði (vhm 26).. ........................................................................................................... 21
Figure 7. Mean discharge seasonality for scenario runs compared with the period 1961–
1990 (shown in blue) and the more recent
/media/ces/2010_016.pdf
......................................................................................................... 19
5 Discussion ..................................................................................................................... 21
5.1 An analysis of an extreme case ........................................................................... 21
5.2 A summary of findings and comparison to other studies
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
...................................................................................................................................................................... 74
Nawri, N. and Björnsson, H.
Surface Air Temperature and Total Precipitation Trends for Iceland in the 21st Century ..................................... 76
Räisänen, J.
Probabilistic projections of temperature and precipitation change for the period 2021-2050 ............................... 78
HYDROLOGICAL PROJECTIONS, RUNOFF
Beldring, S
/media/ces/ces-oslo2010_proceedings.pdf
average of
the volumes given by Equation (5) with the coefficients for ice caps and valley glaciers, respec-
tively, with weights chosen based on the relative proportion of each type of ice bodies. It needs
to be kept in mind that this procedure only provides a rough estimate of the total ice volume
stored in the watershed so that details in the derivation of the volume distribution from the area
/media/ces/ces-glacier-scaling-memo2009-01.pdf
uncertainty),
Monte Carlo analysis, multiple model simulation, NUSAP, quality assurance, scenario analysis, sensitivity analysis, stakeholder involvement
and uncertainty matrix. The applicability of these methods has been mapped according to purpose of application, stage of the modelling process
and source and type of uncertainty addressed. It is concluded that uncertainty assessment is not just
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
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Impact of climate and land use change on the hydrology
of a large-scale agricultural catchment
Lieke van Roosmalen,1 Torben O. Sonnenborg,2 and Karsten H. Jensen1
Received 5 December 2007; revised 21 November 2008; accepted 19 January 2009; published 18 March 2009.
[1] This paper presents a quantitative comparison of plausible climate and land use
change impacts on the hydrology of a large-scale
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf