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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
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/
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/
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
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
-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
; 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
....................................................................................... 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
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