21 results were found for 威尼斯人注册送38元注册靠谱-迪士尼3彩乐园软件下载-(✔️网址700bet.net✔️)-威尼斯人注册送38元注册靠谱-现金365官网地址官方-(✔️访问315bet.net✔️)-威尼斯人注册送38元注册靠谱-威尼斯人注册送38元注册靠谱-威尼斯人注册送38元注册靠谱-(✔️访问bet91.net✔️).
hydrology with respect to hydropower
3 / 16
Ahlstrøm et al., 2009
• recent evaluation of the future hydropower potential
(Ahlstrøm et al., 2009)
• bed and surface topography (radar and LiDAR)
• scenarios of ice flow, mass balance and basin delineation
previous work
4 / 16
motivation
Ahlstrøm et al. (2009):
• only one RCM (HIRHAM4)
• limitations in mass balance modelling
CES project:
• 2 months
• conduct
/media/ces/Machguth_Horst_CES_2010.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
represent annual winter precipitation sums calculatedfrom the stations and multiplied by a constant tuning factor. See Table 3 for explanation of the other runs
Table 3. Correlation (r) and root mean square error (rmse) between modelled and measured winter (bw), summer (bs) and net (bn) balancesat Storbreen. bw-m1: reference modelling bw where Psolid when Tair < 1ºC, bw-m2: Psolid when Tair < 3ºC, bs-m1
/media/ces/GA_2009_91A_4_Andreassen.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
), 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
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf
opportunity evaluation
Case studies
NOE Net
SEAS-NVE
Findings of case studies
• Distribution companies generally well
equipped for climate change
– Cabling of all overhead lines well under way
– Distribution boxes in areas with increased risk of
flooding are elevated already
– Salt spray further inland is becoming an increasing
problem for substations and transformers
Cabling in Denmark
/media/ces/James-Smith_Edward_CES_2010.pdf
in MIKE SHE / MIKE 11 in order to
describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3)
Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure
also show major highways, main roads and the topography in the area.
NONAM Summerschool Copenhagen 22-26 August 2011 3
Figure 3 Zoom in on Horsens by area. Hansted å
/media/loftslag/Horsens_case.pdf
in order to reduce hunting
pressure on the disturbance of waterbirds.
Hydrological modelling
A regional groundwater and surface model is constructed in MIKE SHE / MIKE 11 in order to describe
climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3)
Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure
also show major highways
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf