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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/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
the winter, but weakens
and spreads northeast during the summer. The highest wintertime precipitation occurs southwest
10
Figure 3. Seasonal mean fields in winter ((a) and (c)) and summer ((b) and (d)). (a) and
(b): daily precipitation (coloured contours), 500 hPa geopotential height in metres (red
contour lines), and 250 hPa geopotential height (white contour lines). (c) and (d): sea
surface temperature
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
–averaged
modeled ice velocity corresponding to the simulated 2002 ice sur-
face geometry, using A= 6.8× 10−15 s−1 kPa−3 implicitly includ-
ing the basal sliding (in B), and using A= 4.6× 10−15 s−1 kPa−3
and C = 10× 10−15 m a−1 Pa−3 (in (C)). (D) The contribution of
the modeled basal sliding to the velocity shown in (C).
Table 2. Average annual (September 2002 to September 2003;
accuracy ∼2 m a−1
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
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and dead trees
Tree population
Species composition,
age and size
distribution, growth rate
of different species
Potential growth
/media/ces/CES_BioFuels_Flyer_new.pdf
≤
≤
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TTif
TTifTTDDFsnow
≤
>−
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TTif
TTifTTDDFice
Mean annual temperature difference
Difference relative to 1971-2000
Difference between 25% warmest and 25% coldest years
barb2right +1°C (25% warmest)
barb2right -0.7°C (25% coldest)
barb2right +1.7°C
Catchment elevation (m.a.s.l)
Catchment elevation (m.a.s.l)
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/media/ces/Crochet_Philippe_CES_2010.pdf