Journal of Environmental Psycholog
l
, Ume
,
e
Acceptability of travel demand management (TDM) with the aim of reducing private car use is modeled following a hierarchical
set of beliefs. In a two-part model, pro-environmental orientation, problem awareness, personal norm, and willingness to reduce car use
are linked to beliefs about to which extent the specific TDM measure is perceived
/media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
Harbitz, D. Issler, T. Jóhannesson, K. Lied, M. Naaim, F. Naaim-Bouvet and L. Rammer. Comments and improvements by S. Margreth, J.S. Ásgeirsson and N. Nawri.
April 2010: Passage has been made through snow on the road. Súðavík, Súðavíkurhlíð, West fjords. Photo: Þórður Sigurðsson.
News
/about-imo/news/nr/1631
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
cubic kilometers of water), or a total of 540 ± 130 Gt. This corresponds
to 16 ± 4% of the volume of the glaciers around 1890. About half of this mass
was lost from 1994 to 2019 or 240 ± 20 Gt, which is about 9.6 ± 0.8 Gt / year
on average during that period. Vatnajökull has thinned by 45 m on average in
the period 1890–2019, Langjökull by 66 m and Hofsjökull by 56 m. This corresponds
/about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years
balance data from all the ice caps.
REFERENCES
Björnsson, H., Pálsson F., Guðmundsson M. T. and Haraldsson H. 1998. Mass
balance of western and northern Vatnajökull, Iceland, 1991–1995, Jökull, 45,
35–58.
Björnsson, H., Pálsson F. and Haraldsson H. 2002. Mass balance of Vatnajökull
(1991–2001) and Langjökull (1996–2001), Iceland. Jökull, 51, 75–78.
Bromwich, D. H., Bai L. and Bjarnason G. G. 2005
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf
ÁRSSKÝRSL A 2018
2
Á R S S K Ý R S L A 2 0 1 8
3 Frá forstjóra
4 Veðurstofan 2009–2019
12 Náttúrufar
18 Rannsóknir
20 Fjármál og rekstur
22 Ritaskrá starfsmanna
?Veðurstofa Íslands 2019
Bústaðavegi 7–9, 108 Reykjavík
ISSN 2251-5607
Efni ársskýrslunnar var unnið af starfsmönnum
Veðurstofu Íslands
Ritstjórn: Sigurlaug Gunnlaugsdóttir
Hönnun og umbrot: Hvíta húsið
Prentun: Prentmet
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
Research Basins (NRB) International Symposium and Workshop: 12 August - 18 August, 2009, Iqaluit-Pangnirtung-Kuujjuaq : [conference proceedings, field guide] /editors: Kathy L. Young, William Quinton.Toronto: York University, August 2009. bls. 285-289.
Snorrason, Á. & Harðardóttir, J. (2008). Climate and Energy Systems (CES) 2007-2010. A new Nordic energy research project. In O. G. B. Sveinsson, S. M/ces/publications/nr/1936
2004. Further towards
a taxonomy of agent-based simulation models in
environmental management. Mathematics and
Computers in Simulation 64(1):25-40.
Henle, K., W. Kunin, O. Schweiger, D. S.
Schmeller, V. Grobelnik, Y. Matsinos, J. Pantis, L.
Penev, S. G. Potts, I. Ring, J. Similä, J. Tzanopoulos,
S. van den Hove, M. Baguette, J. Clobert, L.
Excoffier, E. Framstad, M. Grodzinska-Jurczak, S.
Lengyel, P
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
to c. 10% increase
Uncertainty related to choice of GCM
• Changing seasonality (2021-2050 vs 1961-1990)
in Sweden
T2m Precipitation Wind speed
Colored lines represent averages over RCMs forced by the same GCM
Gray field is max/min of all RCM simulations
An example of CC in the next few decades
2011-2040
vs
1961-1990
Why are differences between ensemble
members so large?
Winter (DJF)
M
S
L
P
T
2
/media/ces/Kjellstrom_Erik_CES_2010.pdf
between 300–600 m
above mean sea level (mASL), and decreases gradually again at higher elevations. According to
the Köppen classification scheme, this is indicative of the transition from a maritime to a continen-
tal subarctic climate at about an elevation of 300 mASL. The large increase in SAT from winter
to summer at that level leads to decreasing lapse rates during the warm season at lower
/media/ces/2010_005_.pdf