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/media/ces/Kjellstrom_Erik_CES_2010.pdf
by parametric methods. Hydrology Research 39, 425-436.
Jónsdóttir, J. F., Uvo, C. B. (2009). Long-term variability in precipitation and streamflow in Iceland and relations to atmospheric circulation. Int. J. Climatol. 29, 425-436. doi: 10.2166/nh.2008.002.
Lawrence, D., Haddeland, I. Uncertainty in hydrological modelling of climate change impacts in four Norwegian catchments. Hydrology Research
/ces/publications/nr/1943
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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inhabitants, in terms of environmental and health issues.
The Icelandic Meteorological Office (IMO) monitors gas releases from Holuhraun using DOAS and FTIR instruments for the estimation of SO2 flux and amount of other components in the volcanic cloud. The more abundant gases present are SO2, CO2, HCl, HF, H2O.
In the first month and half we had an averaged flux equal to 400 kg/s (~35 kT/d/pollution-and-radiation/volcanic-gas/measurements/
inhabitants, in terms of environmental and health issues.
The Icelandic Meteorological Office (IMO) monitors gas releases from Holuhraun using DOAS and FTIR instruments for the estimation of SO2 flux and amount of other components in the volcanic cloud. The more abundant gases present are SO2, CO2, HCl, HF, H2O.
In the first month and half we had an averaged flux equal to 400 kg/s (~35 kT/d/pollution-and-radiation/volcanic-gas/measurements
inhabitants, in terms of environmental and health issues.
The Icelandic Meteorological Office (IMO) monitors gas releases from Holuhraun using DOAS and FTIR instruments for the estimation of SO2 flux and amount of other components in the volcanic cloud. The more abundant gases present are SO2, CO2, HCl, HF, H2O.
In the first month and half we had an averaged flux equal to 400 kg/s (~35 kT/d/pollution-and-radiation/volcanic-gas/measurements/nr/3036
course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
……………………………………………………………………………………………………………………………………………………………………
6
Figure 1. Flow chart summarizing information and decision flows of an adaptive management inspired
adaptation planning cycle for road transport (at national strategic / tactical level)
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distribution, growth rate
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