-
corded and important data on the deformation of the caldera ac-
quired.
The real-time monitoring and interpretation of geophysical data
were made accessible to the public via the internet. Both automatic
and manually checked earthquake locations were displayed on
maps, updated every five minutes. Also, cGPS time series were
mapped showing deformation in the area.
Scientists followed the course
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens
fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and
scattered habitation. One of the most important plant community on the islands are along the East coast
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens
fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and
scattered habitation. One of the most important plant community on the islands are along the East coast
/media/loftslag/Case_A___Horsens_Fjord.pdf
7
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ea
n
d
is
ch
ar
g
e
(m
3 /
s)
Present: Mean A2: Mean
Station 280001: Upstream Bygholm Lake
0
5
10
15
20
25
30
35
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ax
im
u
m
d
is
ch
ar
g
e
(m
3 /
s)
Present: Max A2: Max
Station 270045: Upstream Lake Nørrestrand
0
2
4
6
8
10
12
14
16
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ea
n
d
is
ch
ar
g
e
(m
3 /
s)
Present: Max A2: Max
/media/loftslag/Horsens_case.pdf
On the northern side a tephra wall rises 20 meters above the water. The ice walls at the southwestern corner of the crater are melting, i.e. at the site of the vent that was active 4 - 6 June. The rate of melting is assumed to be about one cubic meter per second.
Details on the volume of the lake, and possible flooding from it, in a status report issued collectively by the Icelandic Meteorological
/earthquakes-and-volcanism/articles/nr/1884
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
the maximum discharge of jökulhlaup water at the glacier
terminus is estimated as 97 m3 s 1. This jökulhlaup was a fast-rising jökulhlaup as
other jökulhlaups in Skaftá and cannot be described by the traditional Nye-theory of
jökulhlaups. The total volume of flood water was estimated as 53 Gl. The average
propagation speed of the subglacial jökulhlaup flood front was found to be in the range
0.2–0.4 m s 1
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf