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
new methods to evaluate volcanic crises, increase scientific understanding of magmatic processes and improve delivery of relevant information to civil protection and authorities.
For photos of activities see FUTUREVOLC at facebook.
News
2023
2022
2021
/about-imo/news/nr/2751
) 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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/media/ces/CES_BioFuels_Flyer_new.pdf
-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
Access, can be monitored closely on the EUROVOLC website: https://EUROVOLC.eu. The EUROVOLC project can also be
followed on social media through the dedicated #eurovolc and @eurovolc usernames on Twitter and Instagram, and Facebook. Geographical distribution of European volcanoes (red circles): on the
European continents,
plus Canary islands (left) and in overseas countries (right
/about-imo/news/eurovolc
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
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
facebook .Öræfajökull and Skeiðará river bridge in July 2014. The river has left its channel. Photo: Oddur Sigurðsson.Question: Has Öræfajökull erupted in historical times?Answer: Two eruptions are
known, which occurred in 1362 CE and 1727 CE, both explosive. The eruption in
1362 is assessed to have a Volcanic Explosivity Index (VEI) equals to 6 and the
following one in 1727 equals to 4
/volcanoes/about-volcanoes/oraefajokull/q-a/