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• 21. UST_table_SO2_27112014-en

  Health Effects of Short-term Volcanic SO2 Exposure and Recommended Actions The colors in the table indicate the average concentration of SO2 for 10-15 minutes. The health effects depend both on the time of SO2 exposure and SO2 concentration. Health effect limits are defined as the average concentration of SO2 of 350 µg/m 3 for one hour or 125 µg/m 3 for 24 hours. Concentration of SO2 /media/jar/UST_table_SO2_27112014-en.pdf

• 22. VI_2020_004

  -laid with the deposit isopach for the 1362 eruption. ................ 74 Figure 46 Vertical velocity profile for the eruptive mixture (Öræfajökull) ............................. 75 Figure 47 Probabilistic hazard map for a load ≥1.0 kg/m2 (Öræfajökull) ............................... 76 Figure 48 Probabilistic hazard map for a load ≥100 kg/m2 (Öræfajökull) ............................. 77 Figure /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 23. Journal_of_Hydrology_Veijalainen_etal

  precipitation and time of year (an index for available net radiation) (Vehviläinen and Huttunen, 1997). This equation has been calibrated and verified against observations of Class A pan evaporation values (Vehviläinen and Huttunen, 1997). The actual evaporation is calculated from potential evapora- tion and the soil moisture deficit. The changes in temperature and precipitation affect /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 24. Wind turbines

  and each spade measures 22 metres in length. When the spades are at their highest position each unit will achieve a height of 77 metres. Like all large structures, wind turbines have an inevitable visual impact. However, a permanent impact on the overall appearance of the environment is not considered high in comparison to other types of power plants. Wind turbines can be easily dismantled, leaving /about-imo/news/nr/2642

• 25. VI_2015_005

  with l l2, containing the region with frequent cyclone activity to the northeast of Iceland. Then, of the total study area, 22% fall into the western sector (itself broken up into 70% ocean and 30% land), 32% in the central sector (77% ocean, 23% land), and 46% in the eastern sector (44% ocean, 56% land). The average seasonal cyclone occurrences over the ocean and land areas in different sectors /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 26. 2010_003rs

  is N197°E. The J21 fault, on the other hand, is more linear but with varying dip. South of the epicentre the fault is vertical but north of it, dip changes to 77°. It is 15.5 km long, strikes N179°E and deepens to the south from 6 km to 9 km. Many other smaller faults in Southwest Iceland that were illuminated by the 2000 activity have also been mapped, including the fault planes of three M~5 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 27. GA_2009_91A_4_Andreassen

  ). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf

• 28. hafisskyrsla_11052011

  Eins og sjá má af meðfylgjandi korti er ísinn næst landi um 77 sjml NNV af Straumnesi, 82 sjml NV af Horni, og 146 sjml N af Skaga. Ekki var unnt að greina ísinn vel sökum lágskýja, en útbreiðsla sést vel á SLAR myndum, sem og á eftirlitsratsjá. Ísdreifar voru að sjá á ratsjá um 1-2 sjómílur frá megin ísröndinni. Gunnar Örn Arnarson Yfirstýrimaður TF-SIF /media/hafis/skyrslur_lhg/hafisskyrsla_11052011.pdf

• 29. The weather in Iceland in 2022

  177 -0.3 Bolungarvík 3.9 0.2 27 125 -0.2 Litla-Ávík 3.6 # 19 27 -0.4 Blönduós 3.5 # 17 19 -0.4 Grímsey 3.4 -0.1 32 149 -0.6 Akureyri 4.3 0.1 29 142 -0.3 Grímsstaðir 1.4 0 36 to 37 116 -0.4 Miðfjarðarnes 3.2 # 13 23 -0.4 /about-imo/news/the-weather-in-iceland-in-2022

• 30. VI_2009_006_tt

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf