the com-
plexity of the hydrological processes through modelling, but its application is usually limited to
the short-range. Although the results demonstrated a great potential for this method, its success-
ful application in real-time will strongly depend on the quality and availability of streamflow
observations, which can be poor or simply missing during periods of variable durations, e.g
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
” The latter is in our case
a policy decision represented by point z in Fig. 1. In
European water management, typical policy
decisions that involve participation include water
management plans.
Leading up to the policy decision is the participation
process, represented by the space between points y
and z, in which stakeholders interact with each other
but also with the agency responsible
/media/loftslag/vonKorff_etal-2010.pdf
) is considered as a sequence of steps
corresponding to n individual glaciers of different sizes (with volumes vi and areas si for i = 1
to n), or using
V (v) =
Z v
0
1
g
dS
ds
dx ; (7)
where the slope of the area distribution function, dS=ds, is considered as a function of ice vol-
TóJ 5 5.12.2009
Memo
0 50 100 150 200
0
5
10
15
20
25
Cumulative area (km2)
Area
(km
2 )
0 5 10 15
0.
0
0.
5
1.
0
1.
5
2.
0
2.
5
/media/ces/ces-glacier-scaling-memo2009-01.pdf
to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.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
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009
ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost
operating manage- ment develop- poned-, of land grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation
/media/loftslag/Traffc-maintenance_expenditures.pdf
(-33%) during 1970 to 2004 has been smaller than the com-
bined effect of global income growth (77%) and global population
growth (69%); both drivers of increasing energy-related CO2 emis-
sions. The long-term trend of declining CO2 emissions per unit of en-
ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM}
Differences in per capita income, per capita emissions and
energy
/media/loftslag/IPPC-2007-ar4_syr.pdf
) of the forthcoming changes are
uncertain. This uncertainty comes from three basic sources:
z Scenario uncertainty: future changes in the atmospheric composition, and thus the
external forcing of the climate system, depend on the magnitude of future anthropogenic
emissions of greenhouse gases and other radiatively active substances such as aerosol
particles and their precursor gases.
z Modelling
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
&
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/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf