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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
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
between model terrain and DEM are essentially unbiased, with
an average of 2.0 m, and a mean absolute difference of 10.0 m. The largest deviations, with
magnitudes of up to 300 m, are found in regions with the highest variability in actual terrain
elevations, most notably in the central northern part of the island, as well as along the eastern
and southeastern coast, and in the outlying parts
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
and reported a
rate of 1.9 0.4 mm/yr for 1961-2009. For 1993-2009, they found the rate to be 2.8 0.8 mm/yr
and 3.2 0.4 mm/yr for using tide gauge and satellite altimetry data respectively. Beckley et al.
(2010) found the mean sea level rise rate to be 3.3 0.4 mm/yr for 1993-2009 and noted that the
rate of 2004-2008 was only 2.0 0.4 mm/yr. Multiple studies using different methods agree
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
961–975, 2011
966 G. Aðalgeirsdóttir et al.: 20th and 21st century evolution of Hoffellsjökull glacier
Table 1. Specific winter (bw), summer (bs) and net balance (bn) for
Hoffellsjökull in mw.e. a−1. A conservative error estimate is on the
order of 15–20 % for both bw and bs.
Glacier year bw bs bn
1935–1936 2.0 −3.4 −1.4
1936–1937 2.4 −2.1 0.3
1937–1938 1.7 −2.4 −0.6
2000–2001 2.0 −2.1 −0.1
2001
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
(-33%) during 1970 to 2004 has been smaller than the com-
bined effect of global income growth (77%) and global population
growth (69%); both drivers of increasing energy-related CO2 emis-
sions. The long-term trend of declining CO2 emissions per unit of en-
ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM}
Differences in per capita income, per capita emissions and
energy
/media/loftslag/IPPC-2007-ar4_syr.pdf