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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
6 Net downward shortwave radiation flux at the surface .................................... 18
7 Net downward longwave radiation flux at the surface ..................................... 19
8Net downward total radiation flux at the surface............................................ 20
9 Upward sensible heat flux from the ground .................................................. 22
10 Air
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
). Meteorological observations carried
out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor-
ology and surface energy balance data. Analysis ofthe first five years
/media/ces/GA_2009_91A_4_Andreassen.pdf
evapotranspiration decreased by 19% and
22% for the two catchments, showing that the increased
biomass of the vegetation only partly compensated for the
30% reduction in transpiration due to stomatal closure, as a
result of the higher atmospheric CO2 concentration.
[8] The aim of this study is to determine the sensitivity of
the hydrological system to a number of meteorological and
land use factors, which
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
)
is shown. At the margin the grid boxes of the RCAO RCM are
visible. The area between Illulisat and Swiss camp is commonly
called Paakitsôq.
respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located
on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and
Box, 2001). The locations of the stations are indicated in Fig. 1, further details
/media/ces/ces_geus_paakitsoq_full_report.pdf
Integrated
• Infrastructure
• Large size, indivisibilities, layers, network effects
• Long lifetime, economic & spatial structuring
• Public good features, implications of market organization
8/26/2011Adriaan Perrels/IL 3
26.8.2011Adriaan Perrels/IL 4
Climate change impacts – temporal profiles
Duration of the state resulting from the change* Temporal profile of
the
unfolding of the
change
/media/loftslag/Perrels-CBA.pdf
data, models or analyses, then
the following scale of confidence levels is used to express the assessed chance of a finding being correct: very high confidence at least 9 out
of 10; high confidence about 8 out of 10; medium confidence about 5 out of 10; low confidence about 2 out of 10; and very low confidence less
than 1 out of 10.
Where uncertainty in specific outcomes is assessed using expert
/media/loftslag/IPPC-2007-ar4_syr.pdf
of how climate change will
impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources
and taking advantage of the local tempered climate for keeping the
supercomputer components cool, the running costs and CO2 footprint
will be kept to a minimum, saving tonnes of CO2 in line with the
four nations' efforts towards reaching Net/about-imo/news/joining-forces-in-weather-forecasting-and-climate-research
of the glaciers. An up to 8 m thick winter snow layer
was measured in the accumulation area (∼4 m w.e.). Ice melt
of up 10 m w.e. was measured in the lowest part of the ab-
lation zone in summer, and 2 m w.e. was melted during win-
ter. Taking into account ∼2 m of annual rainfall, the runoff
from this part of the glacier was estimated as ∼14 m w.e. per
year; a surprisingly high value (Ahlmann, 1939
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf