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data, models or analyses, then
the following scale of confidence levels is used to express the assessed chance of a finding being correct: very high confidence at least 9 out
of 10; high confidence about 8 out of 10; medium confidence about 5 out of 10; low confidence about 2 out of 10; and very low confidence less
than 1 out of 10.
Where uncertainty in specific outcomes is assessed using expert
/media/loftslag/IPPC-2007-ar4_syr.pdf
obser-
vations. ................................................................................................ 16
6 Number of records as a function of the total cloud cover. ................................ 17
7 Total cloud cover. Automatic records as a function of manual observations. ........ 17
8 Records from the manual station. When every record over 20 km has been
mapped to the range
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
..................................................................................... 7
2.3 Meteorological data ................................................................................ 8
2.4 Other data ............................................................................................ 8
3 Index flood method ...................................................................................... 11
3.1 General
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
of W-Strandartindur and the gullies
below .................................................................................................. 23
4.5 Areas 7 and 8: Botnabrún ........................................................................ 24
4.6 Areas 9 and 10: Nautaklauf and Klauf ........................................................ 24
5 Assessment of the hazard potential
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
................................................................................................................... 8
Liss M. Andreassen, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen ..................... 9
Lidar measurements of Norwegian glaciers – an overview
Neil Arnold* and Gareth Rees .............................................................................................. 10
Calculation of glacier velocity from repeat
/media/vatnafar/joklar/Reykholt-abstracts.pdf
to be simple and therefore has important drawbacks.
Future improvements should be made in the light of applications within a larger toolbox of scenario
methods.
2008 Elsevier Ltd. All rights reserved.
* Tel.: +31 317 482422; fax: +31 317 419000.
E-mail address: kasper.kok@wur.nl.
Contents lists available at ScienceDirect
Global Environmental Change
journa l homepage: www.e lsev ier .com/ locate
/media/loftslag/Kok_JGEC658_2009.pdf
) Survey indicated that more than half of the respondents in 13 out of 24
countries worldwide felt that climate change was a serious problem (Brechin, 2003,
p. 109). Of these 13 nations, 8 were European (and 5 formed part of the EU15); the
USA did not figure in these 13. More than 65% of the surveyed populations in the
same 23 out of 24 nations indicated they felt that global warming was a serious
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf