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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
). Meteorological observations carried
out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor-
ology and surface energy balance data. Analysis ofthe first five years
/media/ces/GA_2009_91A_4_Andreassen.pdf
and direction, as well as air temperature, from the IMO operational surface station net-
work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some
stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m.
3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary
data file: grib_set -f -d 0.0 -w
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
of Norwegian glaciers – an overview
Liss M. Andreassen*, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen
Section for glaciers, snow and ice, Norwegian Water Resources and Energy Directorate (NVE)
* Corresponding author, e-mail: lma (at) nve.no
ABSTRACT
The current glacier monitoring programme in mainland Norway includes direct mass balance
investigations on 14 glaciers. Accurate maps
/media/vatnafar/joklar/Reykholt-abstracts.pdf
Grin’s work on this article was part of the programme of the
Dutch Knowledge network on System Innovations (KSI).
P. Huntjens (&) C. Pahl-Wostl
Institute for Environmental Systems Research,
University of Osnabruck, Barbarastraße 12, Geb. 66,
49069 Osnabruck, Germany
e-mail: patrickhuntjens@yahoo.com
J. Grin
Amsterdam School for Social Science Research,
University of Amsterdam, Amsterdam
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.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
PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN AND USA
PERSPECTIVES
IRENE LORENZONI and NICK F. PIDGEON∗
Centre for Environmental Risk and Tyndall Centre for Climate Change Research, Zuckerman
Institute for Connective Environmental Research, School of Environmental Sciences, University of
East Anglia, Norwich NR4 7TJ, UK
E-mail: i.lorenzoni@uea.ac.uk
Abstract. If uncontrolled, human influences
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
Franz Josef Land. The western boundary
at 71 W excludes Hudson Bay and Foxe Basin, both associated with their own storm climate.
Baffin Bay is included in its entirety, since storm activity in that region is closely linked to that
over the western North Atlantic (Dacre & Gray, 2009). The eastern boundary at 55 E is chosen
to completely include the Barents Sea. This results in an area of 21,625,566
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf