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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/media/ces/esa_flyer_new.pdf
FOREST BIOMASS FOR ENERGY PRODUCTION –
POTENTIALS, MANAGEMENT AND RISKS UNDER CLIMATE CHANGE
Ashraful Alam, Antti Kilpeläinen, Seppo Kellomäki
School of Forest Sciences,
University of Eastern Finland, Joensuu
F t Cli t d R bl E I t Ri k d Ad t tiu ure Cl ma e an enewa e nergy – mpac s, s s an ap a on
Oslo, Norway
2 June, 2010
Contents
• Forestry in Finland
• Challenges
• Objectives
/media/ces/Alam_Ashraful_CES_2010.pdf
regional flood frequency curve or
growth curve (qR(D;T )) at each site of interest, after proper rescaling by the so-called index
flood, µi(D), of the target site:
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bQi(D;T ) = µi(D)qR(D;T ); (1)
where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged
over duration D, for a given site i. The mean of the AMF series for given duration D is used
here to define
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
activities.
Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe “
University of Oslo Droughts WTs SummaryRelationsIntroduction Outlook
Hydrological drought in NW-Europe: Data
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/media/ces/AnneFleig_May2010_CES.pdf
maps for 1971-2000
Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson.
Reference:
Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model
/weather/articles/nr/1625
and Chemistry of the Earth, Special Issue: COST Action (Accepted for publication).
Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Filling gaps in measured discharge series with model-generated series. Technical Notes. Journal of Hydrological Engineering, 13, 9, 905-909.
Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Trend analysis in Icelandic discharge, temperature and precipitation series
/ces/publications/nr/1943
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Each bar
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range over
whole UK
spatial
area
June 2010 13
Is the impact similar over the
whole UK?
• Changes in the summer minimum rating, i.e.
worst-case conditions – max temperature:
Rating at baseline period 1961
/media/ces/Cradden_Lucy_CES_2010.pdf
Results
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Max snow depth
Trend slope
Number of snow days
Period II
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Max snow depth Number of snow days
Norwegian Meteorological Institute met.no
Correlation analysis (1961-08)
138 mutual stations
Introduction Data & Methods Results
Correlation with
winter
temperature
Correlation with
winter
precipitation
In warmer regions both snow
parameters
/media/ces/Dyrrdal_Anita_CES_2010.pdf