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
) 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
of Ólafsvík is to the left. The fracture line of the avalanche on 19 March 2012 is visible near the top of the slope to the right in the photograph and the avalanche tongue extends to the foot of the slope below the fracture line (this is where the lower part of the hillside is whiter than elsewhere). The fracture line extends into the supporting structures at the location of the topmost row and extends
/about-imo/news/bigimg/2476
of Ólafsvík is to the left. The fracture line of the avalanche on 19 March 2012 is visible near the top of the slope to the right in the photograph and the avalanche tongue extends to the foot of the slope below the fracture line (this is where the lower part of the hillside is whiter than elsewhere). The fracture line extends into the supporting structures at the location of the topmost row
/avalanches/articles/bigimg/2475
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
isobars signify the air pressure, in millibars, at the ocean surface (1 mb = 1 hPa).
The red, purple and blue isotherms show the temperature at 2 m above the ocean surface. A blue line denotes sub-freezing conditions; a purple line denotes 0°C and; a red line denotes temperatures above freezing.
Wind speed is displayed in metres per second (m/s).
The angle of the wind barb is indicative
/weather/articles/nr/1218
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/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf