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21. VI_2020_005

and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

22. Mapping runoff

of the Nordic power-research funds within the project Weather and energy (2003-2006), which the reseach- and educational foundations in the Nordic countries and the Baltic countries participated in. Among the products are a number of maps that are based on an array of climate conditions and hydrological modelling and show water-farming based on conditions now and in the future (Beldring et al,. 2006 /hydrology/runoff/

23. Sea ice in December 2009

2009 Sea ice in December 2009 December 18th two reports from ships were issued about an iceflake located approximately /sea-ice/monthly/2009/nr/2334

24. Gyrite_Brandt_(Local_Government_Denmark,_DK)

and this was done by stakeholder involvement with different levels of involvement. The climate adaptation plan has been presented to the general public and has been used as a basis for integrating climate adaptation measures in the Municipal plan. Lolland is now an pilot study area for two Interreg projects SUSCOD and BLAST, both dealing with the coastal zone and climate adaptation. /media/loftslag/Gyrite_Brandt_(Local_Government_Denmark,_DK).pdf

25. norsem_mantyniemi_poster

Macroseismic maps for two border crossing earthquakes in northern Europe Päivi Mäntyniemi1, Darina Buhcheva2 and Björn Lund2 1Institute of Seismology, Department of Geosciences and Geography, University of Helsinki, Finland 2Department of Earth Sciences, Uppsala University, Sweden We present macroseismic maps for two recent earthquakes that occurred in Sweden and were felt also /media/norsem/norsem_mantyniemi_poster.pdf

26. Skaftá: a glacial outburst flood in progress

cauldron, so travellers on Vatnajökull should stay away from the region, including the lower part of Skaftárjökull and Tungnárjökull, where floodwater could burst through the surface. Background Floods in Skaftá are sourced from two ice cauldrons, formed due to persistent geothermal activity beneath Vatnajökull. On average, the cauldrons drain every two years, producing floods of up to 1,500 /about-imo/news/nr/2819

27. Warning - glacial outburst flood at Skaftá

around the ice cauldron, so travellers on Vatnajökull should stay away from the region, including the lower part of Skaftárjökull and Tungnaárjökull, where floodwater could burst through the surface. Background Floods in Skaftá are sourced from two ice cauldrons, formed due to persistent geothermal activity beneath Vatnajökull. On average, the cauldrons drain every two years, producing floods /about-imo/news/nr/3146

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