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• 21. Sea ice in January 2010

  of Hornstrandir at the following locations: 66°23N - 21°59V and 66°25N - 22°11V. The ice retreated and melted the following days, and the 18th the ice-edge was 8,5 nm N of Geirólfsgnúpur. In the following days the ice retreated further and moved W wards. Over 20 observations from ships were reported and 3 from land. Information on the location of the ice-edge was issued 15 times from IMO. Westerly winds /sea-ice/monthly/2010/nr/2336

• 22. Sea ice in June 2009

  that sparse ice was to be found within the ice-edge. The information also indicated that the ice-edge came closest to shore about 55-75 nm westnorthwest of the Westfjords. A dispatch regarding icebergs was received by the end of the month, but they were at 66°40N and 25°30W. Information regarding the ice-edge was issued four times by the Met office and the Office also received a photograph, taken from /sea-ice/monthly/2009/nr/2328

• 23. 2010_005_

  /media/ces/2010_005_.pdf

• 24. Possibly the largest jökulhlaup

  in the lower reaches of Skaftárdalur during the early hours of Saturday, 3 October. Radio contact still exists with the GPS station in the eastern ice-cauldron; the latest measurements show over 66 m of subsidence since 18:00 GMT on 27 September. During the last one to two hours the rate of subsidence has decreased, suggesting that outflow from the cauldron has peaked. The map below illustrates where /about-imo/news/nr/3207

• 25. 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

• 26. hafisskyrsla_18ag2011

  umferð út af Vestfjörðum. Flugskýrsla TF-SIF 18. ÁGÚST 2011 Flug nr. 10611.025 Kl. 1320 Borgarísjaki á stað 67°18N – 025°42V stakir litlir jakar í grend sjást illa á ratsjá. Kl.1320, tveir borgarísjakar á stað: 67°15N – 025°08V Litlir ísjakar í grend sjást illa á ratjá. Kl.1332, borgarísjaki sirka 100mtr hár og breidd 160 mtr. á stað: 66°40N /media/hafis/skyrslur_lhg/hafisskyrsla_18ag2011.pdf

• 27. New article on glacier changes in

  cubic kilometers of water), or a total of 540 ± 130 Gt. This corresponds to 16 ± 4% of the volume of the glaciers around 1890. About half of this mass was lost from 1994 to 2019 or 240 ± 20 Gt, which is about 9.6 ± 0.8 Gt / year on average during that period. Vatnajökull has thinned by 45 m on average in the period 1890–2019, Langjökull by 66 m and Hofsjökull by 56 m. This corresponds /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years

• 28. vhmkerfi_mars_2012

  "W24°0'0"W 66°2 0'44" N 65°5 0'44" N 65°2 0'44" N 64°5 0'44" N 64°2 0'44" N 63°5 0'44" N 63°2 0'44" N 0 5025 km ¨ VATNSHÆÐARMÆLAR VEDURSTOFU ÍSLANDS 2011 Veðurstofa Íslands IDK 2011Vatnagrunnur birtur með leyfi Landmælinga Íslands Flokkun CA Rennslisstöð CB Vatnsborðsstöð CA Rennslisstöð, FlóðavöktunCB Vatnsborðsstöð, FlóðavöktunW Virkjun eða inntakslónD GunnvatnsstöðVatnasvið /media/vatnafar/maelar/vhmkerfi_mars_2012.pdf

• 29. HARMONIE - numerical weather prediction model 

  of HARMONIE at IMO The current (autumn 2015) set up of HARMONIE is as follows: HARMONIE version 38h1.2 Domain includes 500x480 horizontal grid points, horizontal resolution 2.5 km, see Figure 2. 65 layers in the vertical, top layer at 10 hPa (~30 km a.g.l.) Simulations are performed four times a day Forecasts length 66 hours, time interval of output 1 hour More information on HARMONIE /weather/articles/nr/3232

• 30. CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction

  of climate change on the routine and periodic maintenance of roads. Helsinki 2009. Finnish Road Administration, Central Administration. Finnra reports 8/2009, 66 p. + app. 8 p. ISSN 1459-1553, ISBN 978-952-221-172-9, TIEH 3201122-v. (in Finnish, abstract in English) [5] Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P., Haapala, J., Jylhä, K., Tolonen-Kivimäki, O., and Tuomenvirta, H /media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf