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• 31. The

  in Akureyri in April and June. August was sunny but sunshine duration was close to normal during the other months of the year. Sea level pressure The annual average in Reykjavík was 1005.2 hPa, 0.7 below the 1961 to 1990 mean. The absolute highest pressure of the year was measured at Reykjavík airport on 1 January, 1041.0 hPa, but the lowest at Gufuskálar in the West on 24 February, 951.7 hPa /about-imo/news/the-weather-in-iceland-in-2017

• 32. Isskyrsla_20100407

  N66°44.92' W025°08.94' 79. N66°45.01' W025°08.50' 80. N66°46.32' W025°10.27' 81. N66°46.73' W025°07.19' 82. N66°46.01' W025°04.86' 83. N66°46.22' W025°04.33' 84. N66°47.12' W025°06.45' 85. N66°47.26' W025°04.36' 86. N66°48.44' W025°03.60' 87. N66°49.10' W025°04.45' 88. N66°51.68' W025°03.27' 89. N66°53.36' W024°59.25' 90. N66°55.39' W024°58.89' 91. N66°55.82' W024°58.13' 92. N66°56.15' W025°01.15 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 33. VI_2013_008

  on the use of analogues. Analogue-based methods have been used with success in streamflow forecasting. They are often referred to as nearest-neighbor methods (Karlsson & Yakowitz, 1987; Galeati, 1990; Akbari et al., 2011). The first step of the technique is to compare a current situation to all past situations collected in an historical archive, according to a set of attributes describing /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 34. Possibly the largest jökulhlaup

  observations, the ongoing jökulhlaup could be the largest to have occurred from the Skaftárkatlar cauldrons. At around 10:00 GMT today, floodwater was also detected in Skaftárdalur, where the present discharge is ~400 m³/s and rising quickly; see photos from Búland nearby. At Sveinstindur, the discharge level is in excess of 1,300 m³/s and rising. The jökulhlaup will likely reach maximum discharge /about-imo/news/nr/3207

• 35. Hafisskyrsla_20122010_lhg

  Hafísskýrsla TF-SIF 20. desember 2010 Flug nr. 17910.025 Ískönnunarflug 20. desember 2010 Í dag var farið í ískönnunarflug um vesturmið. Komið var að hafís norður af vestfjörðum, og meginísinn kortlagður með eftirlitsbúnaði flugvélarinnar. Hér að neðan má sjá afrakstur eftirlitsins. Kl.1005, strandaður borgarís 27 sjml ASA af Horni. Staður: 66°22´N-021°19´W /media/hafis/skyrslur_lhg/Hafisskyrsla_20122010.pdf

• 36. BIHU_windrose_2005-2014

  3 3 12 1 4 3 11 3 1 12 2 Wind rose BIHU April 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 12 14 Frequency of wind direction (%) Aerodrome Total observations: 291 Calm: 8.9% Variable winds: 0% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 /media/vedur/BIHU_windrose_2005-2014.pdf

• 37. The weather in Iceland in 2020

  to the 10-year average. It was relatively warmer in coastal areas but colder in the inland.JuneJune was warm and favorable. It was relatively warmest in the Northeast but cooler in the southwestern part. Wind and precipitation were close to average.July July was rather cold compared to recent years, although the mean was above the 1961 to 1990 average. Yet the weather was not unfavorable /about-imo/news/the-weather-in-iceland-in-2020

• 38. VI_2020_008

  by the Peak-over-Threshold with MLE applied on daily and 24-hour accumulated precipitation from the ICRA. ............................... 58 8 Glossary 1M5 – Daily or 24-hour precipitation return level with a 5-year return period AMS – Annual Maxima Series CC – Closeness Coefficient CDO – Climate Data Operator EVA – Extreme Value Analysis GP – Generalized Pareto ICRA – Icelandic /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 39. hafisskyrsla_18ag2011

  – 026°19V. 75 sjóm. NV- af Kópanesi. Kl.1337, tveir borgarísjakar á stað: 66°50N 027°21V. Flugskýrsla TF-SIF 18. ÁGÚST 2011 Flug nr. 10611.025 Kort af ísjökunum út af Vestfjörðum. Flugskýrsla TF-SIF 18. ÁGÚST 2011 Flug nr. 10611.025 Kl. 1400 AIS umferð út af Vestfjörðum og Breiðafirði. Auðunn F /media/hafis/skyrslur_lhg/hafisskyrsla_18ag2011.pdf

• 40. New article on glacier changes in

  to approx. 1890 and create a time series of the volume and mass changes of the glaciers that spans about 130 years.The results clearly show that the average mass loss of the Icelandic glaciers per unit area is among the highest of the main glacierized areas of the world, outside of Antarctica and Greenland. Such glaciers are now rapidly losing mass all over the Earth, causing rising sea level /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years