the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits
were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes
evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob-
servations
/media/ces/GA_2009_91A_4_Andreassen.pdf
to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.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
............................................................................................ 23
17 From left to right, the horizontal axis has the following SYNOP codes (manual
station): The first is 20, the second is 50,51,58 put together in one group, the
third is 52 and to the right is 54. ................................................................ 24
18 The horizontal axis from left to right shows present weather
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
ORIGINAL ARTICLE
Climate change adaptation in European river basins
Patrick Huntjens • Claudia Pahl-Wostl •
John Grin
Received: 1 July 2008 / Accepted: 24 December 2009 / Published online: 2 February 2010
The Author(s) 2010. This article is published with open access at Springerlink.com
Abstract This paper contains an assessment and stan-
dardized comparative analysis of the current water man
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
period, and
linear trends in degrees per decade within the 2004–50 period, for the IPCC GCM
ensemble mean, the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. 23
2 Mean annual surface air temperature and total precipitation during the 1961–90
control period. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 24
3 Dependence on terrain elevation of surface air temperature
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