Occasional Paper no. 20, Center for
International Forestry Research, Bogor, Indonesia.
Pelosi, C., M. Goulard, and G. Balent. 2010. The
spatial scale mismatch between ecological
processes and agricultural management: Do
difficulties come from underlying theoretical
frameworks? Agriculture, Ecosystems and Environment
139(4):455-462.
Pierre, J., editor. 2000. Debating governance:
authority
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
an important part of the runoff from many areas. In total, approximately
20% of runoff in Iceland originates from groundwater (Hjartarson, 1994a).
In the above mentioned previous simulation of runoff map for Iceland for the period 1961–
1990, groundwater was omitted. Effects of groundwater flowing across watershed
boundaries were simulated by scaling the precipitation for each watershed. On watersheds
/media/ces/2010_017.pdf
Bárðarbunga update 29082014
2014-08-29 16:20 UTC
Bárðarbunga update
Compiled by
Icelandic Met Office and University of Iceland Þórður Arason (Ed.)
Based on
Seismic, GPS, Hydrology, Radar, Webcam, PIREP, visual observations
Eruption plume
Height (a.s.l.)
No plume was detected by radar (detection limit above 1 km) and webcam indicated low level
gases and steam from lava fountains during the night
/media/jar/Bardarbunga_Daily_status_report_290814.pdf
Based on a report by
Verta et al. (2007)
92.
5
93.
0
93.
5
94.
0
94.
5
95.
0
M A MJ F J J A S O N D
Mean 19702000
Min and max 1970–2000,
natural rating curve
Target water level zone 1
Target water level zone 2
Q=+20%
Q=+10%
Q= 0%
Q=15%
Q=30%
92.90 m snow target 1
92.70 m snow target 2
Water level (m
)
Month
the regulation limits Lake Syväri has target water level zones, which are not legally
/media/ces/Water_resources_man_Veijalainen_etal.pdf