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
from 5
years of continuous GPS measurements in
Iceland, submitted to Journal of Geophysical
VOLUME 86 NUMBER 26
28 JUNE 2005
PAGES 245–252
Eos, Vol. 86, No. 26, 28 June 2005
EOS, TRANSACTIONS, AMERICAN GEOPHYSICAL UNION
PAGES 245, 248
Forecasting and Monitoring a
Subglacial Eruption in Iceland
Fig. 1. (a) Map of Iceland illustrating the location of monitoring networks discussed in the text
/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
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
of 10-m wind speed in January ................................... 25
17 Average diurnal cycles of 10-m wind speed in July........................................ 26
18 Monthly averages of 10-m wind speed, as a function of terrain elevation ............ 27
19 Monthly mean fields of 10-m wind speed .................................................... 28
20 Monthly variability of 10-m wind speed
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
; fax: +358 20 490 2590.
E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen).
Journal of Hydrology 391 (2010) 333–350
Contents lists available at ScienceDirect
Journal of Hydrology
journal homepage: www.elsevier .com/ locate / jhydrol
Author's personal copy
narios from GCMs or RCMs, and with different emission scenarios
(e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
about 28% and losses from the polar ice sheets
contributing the remainder. From 1993 to 2003 the sum of these
climate contributions is consistent within uncertainties with the total
sea level rise that is directly observed. {WGI 4.6, 4.8, 5.5, SPM, Table
SPM.1}
Observed decreases in snow and ice extent are also consistent
with warming (Figure 1.1). Satellite data since 1978 show that an-
nual average
/media/loftslag/IPPC-2007-ar4_syr.pdf