lágu frá aðal ísnum og náðum að meta
þéttleikann þar. Ekki sáust neinir borgarísjakar né stakir ísjakar í þessu flugi.
Aðalrönd íssins lá í gegnum eftirtalda punkta (tekið með radar). Að sjá var ísinn samfrosta 10/10
1. 66°13,7‘N – 025°35,7‘V
2. 66°24,0‘N – 024°26.0‘V
3. 66°50,1‘N – 023°44,1‘V
4. 67°03,1‘N – 023°31,0‘V
5. 67°00,7‘N – 023°11,3‘V
6. 66°58,7‘N – 022°39,7‘V
7. 66°55,8‘N – 022°23,5‘V/media/hafis/skyrslur_lhg/Isskyrsla_06Jan_2010.pdf
EA Analyse A/S and Optensys
Energianalys will forecast energy system variables, while SINTEF Energy Research will make
assumptions for the energy system in different cases, include new inputs in the EMPS model and
carry out simulations.
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/media/ces/ces_SA_group_flyer_new.pdf
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Figure 1. Scenario building for AWM in Horsens Fjord
To estimate of the adaptation strategy (Table 2) we will use back-casting approach. The assessments
of the productivity of this approach are based on main big strategies which need to have an attention.
One of them
/media/loftslag/Group-1_Scenarios-for-AWM.pdf
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Oddur Sigurðsson, Óðinn Þórarinsson, Philippe Crochet, Tómas Jóhannesson & Þorsteinn Þorsteinsson (2012). Floods in Iceland. In: Z. W. Kundzewicz (ed), Changes in Flood Risk in Europe. Oxfordshire: IAHS Special Publication 10, 257-276.
Hálfdán Ágústsson & Haraldur Ólafsson (2012). The bimodal downslope windstorms at Kvisker. Meteorology and Atmospheric Physics 116(1-2), 27-42, doi:10.1007/s00703
/about-imo/arctic/completed-projects/publications/