is N197°E. The J21 fault, on the other hand, is more
linear but with varying dip. South of the epicentre the fault is vertical but north of it, dip
changes to 77°. It is 15.5 km long, strikes N179°E and deepens to the south from 6 km to 9
km. Many other smaller faults in Southwest Iceland that were illuminated by the 2000
activity have also been mapped, including the fault planes of three M~5
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
An ice edge was observed in the area from 67°31'N and 023°35'W to 66°41'N and 23°43'W. Westerlies were a little more prevailing in the Greenland Strait and north of Iceland than on average
/sea-ice/monthly/2010/nr/2340
) and changing climate (CC:CC)
1. Current climate (CU)
- varying thinning regimes
(0%, 15%, 30%,45%)
2. Changing climate (CC)
- varying thinning regimes
(0%, 15%, 30%,45%)
3. Current (CU) &
changing climate (CC)
- current thinning regime
4. Current (CU) &
changing climate (CC)
- changed thinning regimes
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/media/ces/CES_BioFuels_Flyer_new.pdf
in sea-ice and snow sesearch
Allen Pope, Ian C. Willis, Finnur Pálsson, Neil S. Arnold1, W. Gareth Rees and Lauren
Grey ......................................................................................................................................... 31
Elevation change, mass balance, dynamics and surging of Langjökull, Iceland from 1997 to
2007
Peter Rieger
/media/vatnafar/joklar/Reykholt-abstracts.pdf
of market organisation alternatives
26.8.2011Adriaan Perrels/IL 10
Cost-benefit analysis – the basics 3
Simple example: despite positive IRR still cash flow challenge years 1 - 8
CBA example - initial investment 100; interest and discount 5%;
operational cost +5%/y; benefits +10%/y; IRR = 7.4%
-20
-10
0
10
20
30
40
50
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15
years
m
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writing off
finance
/media/loftslag/Perrels-CBA.pdf