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....................................................................................... 10
3 September 2012 .................................................................................. 12
3 Radiation fluxes at the surface ....................................................................... 16
4 Heat fluxes at the surface .............................................................................. 21
5 Net energy
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.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
)
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
), it was decided to broaden the remit to include both mitigation and adaptation
measures across the broad range of transport systems.
Expected main climate effects for Finland in relation to the national road network: 1)
Wetter winters with lower snowfall and more rain, 2) increase in freeze/thaw cycles in
winter in the southern parts of Finland, 3) higher frequency and severity of storms, 4)
hotter
/media/loftslag/Group4.pdf
and manyof the individual snow falls in late summer (Fig. 4).However, much of the variability in the winter sea-
son was not reproduced by the model, but thesealbedo fluctuations have little impact on the net bal-
ance as the energy available for melt is seldom pos-itive in the winter months. Ice albedo was assumedto be constant, a value of 0.30 was chosen. Meas-urements from the AWS as well as the point
/media/ces/GA_2009_91A_4_Andreassen.pdf
-corrected SPOT 5
high-resolution geometric (HRG) images with 2.5 m
2.5 m spatial resolution, acquired in the autumn 2003
and (4) airborne polarimetric synthetic aperture radar
images observed simultaneously to the 1998 EMISAR
images and the EMISAR DEM viewed as a shaded
relief image (Magnu´sson et al. 2005b).
We estimate the average specific net mass balance (in
m yr1 w. eq.) as
bn r
DV
A1 N
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
Assessment Re-
port (AR4).
Topic 1 summarises observed changes in climate and their ef-
fects on natural and human systems, regardless of their causes, while
Topic 2 assesses the causes of the observed changes. Topic 3 pre-
sents projections of future climate change and related impacts un-
der different scenarios.
Topic 4 discusses adaptation and mitigation options over the
next few decades
/media/loftslag/IPPC-2007-ar4_syr.pdf
and Relative Changes When Comparing the A2
and B2 Scenarios to the Current Climatea
Scenario Net Recharge Horizontal Boundary Outflow Drain Flow Base Flow Water Supply Irrigation
Simulations Not Including Abstractions and Irrigation
Current climate 550 23 279 252
A2 scenario + 67 (12%) + 1 (4%) + 56 (20%) + 13 (5%)
B2 scenario + 113 (21%) + 1 (4%) + 92 (33%) + 22 (9%)
Simulations Including Abstractions
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf