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
). NeWater is based on the
hypothesis that IWRM cannot be realised unless current
management regimes undergo a transition towards more
0301-4797/$ - see front matter r 2007 Elsevier Ltd. All rights reserved.
doi:10.1016/j.jenvman.2007.05.009
Corresponding author. Tel.: +45 38 14 27 71; fax: +45 38 14 20 50.
E-mail address: hjh@geus.dk (H.J. Henriksen).
(Downing et al., 2005). Vulnerability
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey
Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann Höskuldsson, Laura Sandri, o.fl.
73
16,0
2020-008
Reassessment of precipitation return levels in Iceland
Andréa-Giorgio R. Massad, Guðrún Nína
/about-imo/publications/2020/
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Each bar
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spatial
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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
the observed data sets are smaller in SW than in NE
• MMM overestimates precipitation, but is closer to observations in SW than
NE barb2right Better observational coverage in SW
SW
NE
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CES Conference, Oslo 31.5.-2.6.2010
SWNE
• Precipitation trends (mm / 10 yr) in 1961-2000 according to observations
and model simulations (MMM)
• Including the range
/media/ces/TietavainenHanna_CES_2010.pdf
A (4), 233-251.
Andreassen, L. M., van den Broeke, M. R., Giesen, R.H., & Oerlemans, j. (2008). A five-year record of surface energy and mass balance from the ablation zone of Storbreen, Norway. Journal of Glaciology, 54 (185), 245-258.
Andreasen, L.M., van den Broeke M.R., Giesen R.H. & Oerlemans J. (2008). A five-year record of surface energy and mass balance from the ablation zone
/ces/publications/nr/1940
as a function of epicentral distance and recalculated magnitude,
here denoted by Mw(v) were analyzed using the R statistical package (R Development Core
12
Team, 2007). The model candidates were fitted using least-squares methods such as lm (linear
model) and nlm (non-linear minimization), which are available in R. Non-linear minimization
(Dennis and Schnabel, 1983; Schnabel et al, 1985
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
in Finland
Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b
a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland
b Department of Geography, FI-20014 University of Turku, Turku, Finland
a r t i c l e i n f o
Article history:
Received 7 January 2010
Received in revised form 13 June 2010
Accepted
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
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
-CALPUFF model is not using plume height estimates
as an input parameter. The model itself solves the equations describing the rising of the mixture
in the atmosphere and calculates the top-plume height by using some physical parameters as
the vertical mixture velocity (V) and the radius of the vent (R). Based on these two parameters,
V and R, we get an estimate of the mass flow rate and we
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf