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• 21. Sea ice in November 2010

  Search Search string Contact IMO © Veðurstofa Íslands | Bústaðavegi 7- 9 | 105 Reykjavík | Phone 522 6000 | Fax: 522 6001 Recording 902 0600 | SSN 630908-0350 Contact us | Employees /sea-ice/monthly/2010/nr/2346

• 22. Sea ice in January 2010

  moved towards the Westfjords in the first week and the 7th IMO issued a warning as the ship passage between Barði and Straumnes could close the following days. However, that did not happen, most likely as the ice melted as it came closer ashore. The 16th the ice-edge was 17,5 nm E of Horn, 12,5 nm N of Drangasker and 16 nm NNE of Þaralátursnes. The 17th two ice bands reach land north /sea-ice/monthly/2010/nr/2336

• 23. 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

• 24. 2010_005_

  Century control runs, as well as 21st Century forecast runs, submitted by various institutions to the Intergovernmental Panel on Climate Change (IPCC) for their Forth 11 Table 1. General circulation and regional climate models that were considered in this study. Model Version Model Name, Institute BCCR BCM 2.0 Bergen Climate Model, Bjerknes Centre for Climate Research, Bergen, Norway CCCMA CGCM 3.1 /media/ces/2010_005_.pdf

• 25. 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

• 26. 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

• 27. Traffc-maintenance_expenditures

  229 1 587 160 1970 18 591 42 413 2 166 86 101 - 892 5 131 2 310 201 - - - 157 805 1 652 904 1969 17 559 38 840 2 313 93 776 - 922 4 562 1 571 - - - - 159 543 1 832 354 1968 13 474 36 376 3 074 104 519 - 1 080 4 131 1 156 - - - - 163 811 1 964 368 1967 11 139 34 495 5 940 95 857 - 419 3 032 1 087 - - - - 151 968 1 936 249 1966 9 835 32 581 8 349 94 777 - 587 4 205 1 743 - - - - 152 077 2 032 936 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 28. 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

• 29. 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

• 30. vhmkerfi_mars_2012

  W W W W W W W D DD DD DD CB CA CB CA CA CB CB CB CA CA CB CA CA CA CBCB CB CA CB CB CB CBCBCB CB CB CA CA CACA CA CA CACACB CA CA CA CA CB CA CA CA CA CA CB CA CA CA CACA CA CB CA CA CA CA CA CA CB CA CA CA CBCA CA CACA CA CA CA CA CA CA CA CB CA CA CA CBCB CB C CA CA CB CB CA CA CB CA CB CA CA CB CA CA CA CACA CA CB B CA CA CA CA CA CB CA CA CA CA CB CA CA CAC CACB CA CBCB CB CB CB CACA CBCA C B /media/vatnafar/maelar/vhmkerfi_mars_2012.pdf