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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
of events closely.
Photo: Sigurlaug Gunnlaugsdóttir.
Bárðarbunga
Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com-
munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson.
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
5
The magma intrusion from Bárðarbunga
to the eruption site at Holuhraun and
related tremor pulses
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
At 2250 UTC, the plume was detected by the
weather radar at ~8 km height over Vatnajökull,
reaching ~12 km four hours later (Figure 1c).
Lightning over Grímsvötn, which accompanied
the rising plume (Figure 3d), was eventually
seen at ~0300 UTC, but darkness and weather
conditions prevented visual observation of the
eruption site until the following day.
Over the next two days, the strength
/media/jar/myndsafn/2005EO260001.pdf
a systematic com-
parison of results to observed precipitation has been carried out. Un-
dercatchment of solid precipitation is dealt with by looking only at
days when precipitation is presumably liquid or by considering the
occurrence and non-occurrence of precipitation. Away from non-
resolved orography, the long term means (months, years) of observed
and simulated precipitation are often
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
/lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13
April 2009.
[2] WTO, World Tourism Organization (2008): “Climate Change and Tourism -
Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain.
Available at:
http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7
March 2010.
[3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for
sustainable
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
The
precipitation is corrected for wetting and aerodynamic
effects using the standard correction methods of Allerup et
al. [1998]. The average precipitation in the area equals
1073 mm/a. ETref is calculated using the Makkink [1957]
formula, and has an average value of 570 mm/a. The
average annual temperature is 8.2C with a maximum of
16.5C in August and a minimum of 1.4C in January.
[12] The central
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
Differences in terrain elevation between HARMONIE model and DEM............. 12
4 Dependence of temperature and wind speed on model terrain elevation.............. 13
5 Average diurnal cycles of HARMONIE model temperature and wind speed........ 14
6 Absolute mean errors of SURFEX 2-m air temperature and 10-m wind speed ..... 16
7 Average profiles of air temperature and wind speed in January
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf