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Results:

• 1. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 2. 100 years of seismic observations

  with a horizontal short period Willmore seismograph, was installed southwest of the Vatnajökull ice cap. The same type of seismograph was installed in Reykjavík in 1966 and in the east of the country in 1967. In 1968, a new station was installed southeast of Mýrdalsjökull. With these six stations mapping of the main seismically active areas in Iceland was possible. In 1960, IMO was invited to participate /earthquakes-and-volcanism/conferences/jsr-2009/100_years/

• 3. Pollution

  Weather observations began at Stórhöfði in 1921 and since 1940 at night as well. Nine years of age Óskar began keeping a diary on weather and assisting his father. In 1952 Óskar began regular weather observations, in 1953 he began tagging seabirds and in 1966 when his father died Óskar took over both the duties of weather observations and attending the lighthouse. Weather observations were done /pollution-and-radiation/pollution/

• 4. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 5. 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

• 6. 2013_001_Nawri_et_al

  -specific power coefficient, which has a theoretical maximum of 0.593 (Betz, 1966). Practically, however, the power coefficient of modern wind turbines typically has highest values of 0.40 – 0.50, for wind speeds between 5 and 10 m s 1. The effective power curve, i.e., the actual power produced by a given turbine as a function of wind speed, needs to be determined empirically, and is made available /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 7. VI_2020_011_en

  ; Kjartansson, 1966) and Stórhöfði (at least one century older than Sæfjall; 14C method measured on peat; Kjartansson, 1966). Bjarnaey and Elliðaey are also close in age to Sæfjall and Stórhöfði (Jakobsson, 1979) indicating there was a major volcanic episode between 5,000 – 6,000 years BP. Álsey, Brandur, Surðurey, and Hellisey may be about 8000 years BP based on tephrochronology (Jakobsson, 1979 /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 8. VI_2015_006

  ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 9. VI_arsskyrsla2020

  - breytingar komust á dagskrá. Starfsmenn Veðurstofunnar við fyrstu arskiptatölvu stofnunarinnar. Frá vinstri: Sigurjón Magnússon, Stefán Ólafsson, Sigurjón Gestsson og Þórir Sigurðsson (sitjandi). Ljósmynd: Gunnar Hvammdal Sigurðsson. STARFSEMIN FEST Í SESSI m.kr. (verðlag 2008) 0 100 200 300 400 500 1966 1976 1986 1996 2006 Heildarumfang Vatnamælinga 1966-2008 Ríkisframlag Sértekjur ÁRSSKÝRSLA /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 10. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf