not fit the data very well, and results from previous
filters were chosen instead. However, note that this applied to less than 10 cases out of the
401.
Figure 6 – Evolution of the snowpack (black line), accumulated melting (dashed blue
line), and daily runoff (grey bars) for catchment Búðarháls and hydrological year 1995
– 1996. The vertical red line indicates the start date
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
increases by 2.1ºC, and the interannual standard deviation dec-
reases by 6%, when the simulated global mean T increases by 1ºC.
Of course, there is variation between different models!
Time series of winter mean temperature
in Helsinki (1961-2008)
Blue line = observations
Red line = best-estimate present-day (2010) climate
Grey dots = results for individual models
Probability distribution
/media/ces/RaisanenJouni_CES_2010.pdf
frequency distributions for Re-
gion 1 derived with index flood model no. 6: bµ(D) = a(AP=Z)b ............................ 39
5
Appendix VI - Empirical and modeled daily flood frequency distributions for
Region 2 derived with index flood model no. 3: bµ(D) = a(APm)b ......................... 41
Appendix VII - Instantaneous Index flood models for Region 1. .......................... 43
Appendix VIII
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.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
POLICE
DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT
Figure 2 Cross sections of repeated aerial measurements of the subsidence of the Bardarbunga caldera.
NATIONAL COMMISSIONER OF THE ICELANDIC POLICE
DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT
Figure 3 Subsidence of the Bardarbunga caldera from the 16th of August2014. The measurements fit to an exponential
/media/jar/Factsheet_Bardarbunga_20150130.pdf
level 2-3 hours earlier (during peak flow) is seen on the debris-laden ice walls. Two people can be seen on the ice. Photo: Þorsteinn Þorsteinsson.
Measurements at the upwelling
Figure 6. Temperature measurement at the upwelling site. The scientist doing the measurement is connected to a safety line. A temperature recorder lowered into the water stores data in its memory, which later
/about-imo/news/2010/nr/2042
level 2-3 hours earlier (during peak flow) is seen on the debris-laden ice walls. Two people can be seen on the ice. Photo: Þorsteinn Þorsteinsson.
Measurements at the upwelling
Figure 6. Temperature measurement at the upwelling site. The scientist doing the measurement is connected to a safety line. A temperature recorder lowered into the water stores data in its memory, which later
/about-imo/news/nr/2042
of Southwest Iceland ............................................................................... 3
1.2 Historic earthquakes in the SISZ ............................................................................. 6
1.3 The June 2000 earthquakes ..................................................................................... 9
1.4 Crustal structure of Southwest Iceland
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf