) Measured 1997 and 1999 ice surfaces of Lang‐
jökull and Hofsjökull, respectively. c) Steady‐state glacier
geometries after a few hundred year spin‐up with constant
mass balance forcing.
Figure 3: Simulated response of Langjökull (L), Hofsjökull (H)
and southern Vatnajökull (V) to climate change. The inset
numbers are projected volumes relative to the initial stable
ice geometries
/media/ces/ces_flyer_glacierssnowandice.pdf
EA Analyse A/S and Optensys
Energianalys will forecast energy system variables, while SINTEF Energy Research will make
assumptions for the energy system in different cases, include new inputs in the EMPS model and
carry out simulations.
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• Monthly temperature
• Monthly precipitation
Step 2: Extrapolation of model
parameters to all glaciers in
Iceland and Scandinavia
• Gridded climate variables
Step 3: Future projections until
2100 for each glacier:
- run mass-balance model
- Volume-area scaling
Volume-area-length
scaling
V = c Aγ
• Glacier inventory data
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/media/ces/Hock_Regine_CES_2010rs.pdf
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30-year flood
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Flood frequency estimation applied
to annual maximum flood series
% change in
200-year
flood
Projected change in 200-yr. flood
between 1961-1990 and 2021-2050
Change (%)
90th percentile
of 150 models
Median of
150 models
Change (%)
Range of uncertainty in projections
Median of
150 models
Change (%) Range (%)
Range
10 to 90%
Downscaling method
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June 20, 09:00‒10:30 ‒ Lidar instruments and surveying
Peter Rieger
RIEGL Laser Measurement Systems GmbH, Austria
An airborne laser scanner utilizing novel multiple-time-around processing for efficient
wide-area and high point density mapping of mixed-terrain, ice-sheets, and glaciers
Henriette Skourup, René Forsberg, Sine M. Hvidegaard, Indriði Einarsson, Arne V. Olesen,
Stine K. Rose, Louise
/media/vatnafar/joklar/Reykholt-abstracts.pdf
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7 78 Anja Wejs Denmark
Environmental
management
8 93 Tommy Chan Finland Forest sciences
9 140 Karoliina Pilli-Sihvola Finland
E viro me tal
economics
10 147 Jussi Ylhäisi Finland Meteorology
11 (new) Karen Lundgren Sweden
Engineering &
Design
12 (new) Väinö Nurmi Finland Economics
13
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
samfelld byggð hefur verið fast undir brekkunum í rúm 100 ár. Þetta mikla návígi byggðar og
brekku felur í sér að öll umtalsverð ofanflóð á svæðinu ættu að hafa þótt í frásögur færandi og
því ratað í heimildir.
20
4 Ofanflóðasaga
Alvanalegt er að snjóflóð falli í Hlíðarfjalli. Eitt flóð sem sagnir eru um að hafi fallið árið 1952
sker sig nokkuð úr. Ef marka má heimildir féll það úr öllum
/media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
- gróðurhúsaáhrif. Lifandi vísindi, pp. 52-54.
Snorrason, Á. (2002). Veður, vatn og orka. Presented at the Ársfundur Orkustofnunar 2003, Reykjavík, Mar 20. 31-39. [Extended abstract]
Snorrason, Á. (2002). Veðurfar, vatn og orka. Presentation, Aðalfundur Jöklarannsóknafélags Íslands. Norræna húsið, Reykjavík, Iceland. Feb 26. [Presentation]
Snorrason, Á. (2004). The International Hydrological
/climatology/research/ce/publications/