in five-year basis
Current state of the road network affects the possible decisions to be made at the moment
Political adaptation
Management structures have to be more flexible and ready to apply adaptive management
Technological adaptation
0
1000
2000
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4000
5000
6000
1985199019952000200520102015202020252030
vans (mln.
tonkm)
lorries (mln.
tonkm)
0
10000
20000
30000
/media/loftslag/Group3-Road-scenarios.pdf
Vision for Proactive Climate Change Adaptation in the Danish Water Sector
Speaker: Helle Katrine Andersen, DANVA hka@danva.dk
To inspire water utilities to develop climate change adaptation strategies and to implement
CC adaptation solutions The Danish Water and Waste Water Association (DANVA) has
developed a vision for Proactive Climate Change Adaptation in the Water Sector
/media/loftslag/Helle_Katrine_Andersen_(DANVA,_Dk).pdf
) and changing climate (CC:CC)
1. Current climate (CU)
- varying thinning regimes
(0%, 15%, 30%,45%)
2. Changing climate (CC)
- varying thinning regimes
(0%, 15%, 30%,45%)
3. Current (CU) &
changing climate (CC)
- current thinning regime
4. Current (CU) &
changing climate (CC)
- changed thinning regimes
C
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a
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/media/ces/CES_BioFuels_Flyer_new.pdf
Figure 8. Stations ranked according to their average CC for the 20 highest rainfall daily events.
................................................................................................................................................... 33
Figure 9. Ranked values of the 50 highest 24-hour accumulated precipitation events plotted
against ranked values of the 50 highest daily precipitation
/media/vedurstofan-utgafa-2020/VI_2020_008.pdf
The observed travel time differences already mentioned can either be obtained from absolute times of
measured (picked) phase arrivals (logged in earthquake catalogs) or as relative times between phases
measured with cross-correlation (CC) of waveforms. CC between closely spaced earthquakes can give
highly accurate relative time differences between phases, and can correct bad picks from
/media/norsem/norsem_begga.pdf
offshore north Iceland
1.10.2013
Two earthquakes reaching magnitude 3 and 3.2 occurred this morning at 06:14 and 07:41 offshore North Iceland, 10 km NW of Gjögurtá.
They are a part of swarm activity which has been ongoing since September 25. Roughly 1000/about-imo/news/nr/2757
October 2013 off shore North Iceland. Roughly 1000 earthquakes have been recorded in the swarm. Topography of seabed: Bryndís Brandsdóttir, Institute of Earth Sciences, University of Iceland.
News
2023
2022
2021
2020
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2018
2017
/about-imo/news/bigimg/2757
-13
FL180: 270/25-45KT, but 26015KT by the NE-coast, -29
Overview of weather systems:
1000 km S of Cape Farewell is an extensive 980 mb low. Over Greenland is a 1038 mb high.
Near surface winds:
N-ly or variable wind, 05-25 KT.
Cloud heights/visibility/weather:
BKN/OVC at 1000-2500 FT in the N-part and occasional snowshowers with poor visibility. Widely FEW/SCT and good
/weather/aviation/llf-iceland/
mix, 4) mobility patterns,
technological development, 5) equitable distribution of social goods, ethical dynamics
Background information and knowledge gaps: 1) time scale-what is the consensus view
of when are the CC impacts projected to begin to be felt, 2) spatial scale-where are the
impacts expected to occur, 3) vulnerability assessments of differential capacity to adapt
to CC impacts
/media/loftslag/Group4.pdf