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Results:

• 61. 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

• 62. isskyrsla_14122010

  Hafísskýrsla TF-SIF 14. desember 2010 Flug nr. 17610.025 Óformleg ískönnun 14. desember 2010 Óformleg ískönnun var gerð og kom eftirfarandi í ljós. Ísröndin samkvæmt ratsjá TF-SIF 1) 68 03.0N 17 19.0W 2) 67 41.0N 18 19.0W 3) 67 36.0N 19 09.0W 4) 67 21.0N 19 43.0W 5) 66 53.0N 20 21.0W 6) 66 45.0N 19 58.0W 7) 66 38.0N 20 42.0W 8) 67 02.0N 21 /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf

• 63. VI_2020_005

  2 mm/yr in northern Denmark and down to almost 0 mm/yr in the South (Miljø- og Fødevareministeriet / Miljøstyrelsen, DTU Space, and Geodatstyrelsen, 2016). In (figure 1), the land uplift relative to the geoid from the official NKG2016LU land uplift model (Olav Vestøl et al., 2019) that was developed in 2016 and is used in the Nordic and Baltic countries, is shown for the Scandinavian countries /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 64. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 65. ces-oslo2010_proceedings

  anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf

• 66. IPPC-2007-ar4_syr

  a near-zero pre-industrial background concentration, primarily due to human activities. {WGI 2.3, SPM; SROC SPM} There is very high confidence that the global average net effect of human activities since 1750 has been one of warm- ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2 (Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM} The combined radiative forcing due to increases in CO2, CH4 and N2O /media/loftslag/IPPC-2007-ar4_syr.pdf

• 67. Home-page - Icelandic Meteorological Office

  (Icelandic) Apr 16Mikil rigning og leysing á Suðausturlandi Töluverðri rigningu er spáð á Suðausturlandi frá því í kvöld, sunnudag, og fram á mánudag. Spár gera ráð fyrir að það dragi úr ... Apr 16Seyðisfjörður 16.4.2023 Lítil úrkoma hefur verið á Seyðisfirði síðustu /

• 68. Publications

  with observations from Reykjavík, Akureyri, Akurnes, Keflavík, and Hveravellir.Please note that the downloadable DjVu program is needed to view Veðráttan magazine.Veðráttan 2000-2018 is shown on this web-site . Earlier publications: Íslensk veðurfarsbók 1920-1923 = Annuaire météorologique d'Islande Meteorologisk Aarbog 1873-1919. Anden del. Færøerne, Island, Grønland og Vestindien = Annuaire /about-imo/publications/

• 69. Avalanche dams

  in Iceland: Snjóflóð á varnargarðinn við sorpbrennsluna Funa í Engidal við Skutulsfjörð þann 14. janúar 2004 (IMO Memo TóJ-2004-02, author T. Jóhannesson) (pdf 0.3 Mb) Run-up of two avalanches on the deflecting dams at Flateyri, northwestern Iceland. (Annals of Glaciology, 32, 350−354, 2001, author T. Jóhannesson) [abstract] (html) Snjóflóðið á Flateyri 21. febrúar 1999 og áhrif varnargarða /avalanches/imo/dams/

• 70. Pilot reports

  Tengt efni Hjálp Textaspár Veðurþáttaspá Veðurathuganir Orðskýringar Veðurtákn og skýringar /weather/aviation/pirep/