Journal of Social Issues, 56, 407-424.
Von Korff Y, d'Aquino P, Daniell KA, Bijlsma R (2010) Designing participation processes for water management and beyond. Ecology and Society 15(3): 1.
http://www.ecologyandsociety.org/vol15/iss3/art1/
Samuelson CD (1993). A multiattribute evaluation approach to structural change in resource dilemmas. Organizational Behavior and Human Decision Processes
/media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009
ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost
operating manage- ment develop- poned-, of land grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation
/media/loftslag/Traffc-maintenance_expenditures.pdf
750-1170
AAR of the warm year of 2004
- digitized using the October 2004 SPOT 5 HRS images
Ice cap
E: Eyjafjallajökull
To: Torfajökull
Ti: Tindfjallajökull
AAR (%)
20-25
<5
0
Method
References
Berthier E., Arnaud Y., Baratoux D., Vincent C. and Rémy F. 2004. Recent rapid thinning of the "Mer de Glace" glacier derived from satellite optical images.
Geophys. Res. Lett., 31, L17401, doi:10.1029
/media/ces/glacier_mass_balance_poster.pdf
Such landslides fall from a comparatively high
elevation, cause extensive disruption and upheaval of loose materials and soils in their
way, and can travel considerable distances uphill against opposing slopes.
Secondly, there are medium-sized or large, rapid debris flows that are released from com-
paratively high elevations and are confined to gullies as they travel down the mountain-
side, similar
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
and the y-axis the dates between March and July. For every year,
the melt season starting date is plotted (blue dots), and a blue line connects the dates for all the
years. A regression line fitting those values (orange line) is shown, and the difference in days
between the beginning and the end of the period, as calculated from the regression line, is
indicated at the top of the plot.
In 9 cases
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
) storage coefficient of interflow ki; (3) drainage
density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant
krec for the decreasing saturated hydraulic conductivity with increasing depth. For the
groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X and Y
direction. The hydraulic conductivity is adjusted in distributed grids unlike
/media/ces/2010_017.pdf
High-resolution regional
climate simulations over Iceland using polar MM5. Mon. Wea. Rev., 133, 3527–
3547.
Buzzi A., Tartaglione N. and Malguzzi P. 1998. Numerical simulations of the
1994 Piedmont flood: Role of orography and moist processes. Mon. Wea. Rev.,
126, 2369–2383.
Chiao, S., Lin Y.-L. and Kaplan M. L. 2004. Numerical study of the orographic
forcing of heavy precipitation during MAP IOP
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf
Use of relatively located micro-
earthquakes to map fault patterns
and estimate the thickness of the
brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir
VÍ 2010-003
Skýrsla
f l l l dUse o re ative y ocate micro-
earthquakes to map fault patterns
and estimate the thickness of the
brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir, Veðurstofu Íslands
VÍ 2010-003
ISSN 1670-8261
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf