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
Figure 8. Stations ranked according to their average CC for the 20 highest rainfall daily events.
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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
was within the Greelandic jurisdiction but only minimal scattered ice within the Icelandic one. The ice was closest to land about 82 nm NW off Straumnes and 93 nm NNW off Horn.
The Greenland Straight had northeasterly wind directions during the whole month
/sea-ice/monthly/2011/nr/2376
) 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
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-scale natural disaster one would expect that people would
abandon their cars from one day to another.
Political uncertainty – budget uncertainty
Scenario
combination
Impact Adaptation measures
North South North South
A *
CC: Possible increase in the
amount of snow more
snow clearing increase in
operational costs
S-E: increase in traffic volume
increased wear of roads
/media/loftslag/Group3-Road-scenarios.pdf
punktalisti yfir legu ísrandarinnar, sem og myndir úr eftirlitsratsjá
og kort sem unnið var á SLAR ratsjánna.
Á neðangreindri töflu sést lega íssins frá sv-na.
Hafísskýrsla TF-SIF
3. maí 2011
Flug nr. 02911.025
Kl 14:35 ísinn 82 sml NV af straumnesi og á neðri myndinni 105 sjml NNA af Horni.
Hafísskýrsla TF-SIF
3. maí 2011
Flug nr. 02911.025
Kl.1422 til
/media/hafis/skyrslur_lhg/hafisskyrsla_03052011.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
thickness is 10-12 meters and estimated volume of eruptive material 22-24 million cubic meters (only one fifth of Hekla 2000).
Accordingly, the average flow rate has been approximately 15 cubic meters per second since the eruption began. The eruptive cone stands 82 m above previous ground level and the highest peak is 1067 m a.s.l.
On their web-site, explanatory photographs can be found (pdf 1.1 Mb
/about-imo/news/nr/1862
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