of the volcano, in addition to
vertical subsidence. These observations are consistent with deflation of a magma reservoir
beneath Eyjafjallajökull.
Magma flow: No measurements possible today; however, the intensity of the eruption suggests
that the discharge level is similar to the preceding four days (i.e. 20–40 tonnes s–1).
Other remarks: No measurable geophysical changes within the Katla volcano
/media/jar/myndsafn/Eyjafj_status_2010-04-27.pdf
the Fljótsdalsheiði region . . . . . . . 47
18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48
19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49
20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50
21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51
22 Seasonal mean
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.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
According
to Harpa, the landslide was of a different nature than the landslides that
occurred earlier in the week. "The preliminary observations show a
landslide scar that is up to 20 m high, and it seems to reach deep into
sediments that have not collapsed for millennia. We did not expect a landslide
of this magnitude and we underestimated conditions at the site where the
landslide fell
/about-imo/news/the-landslide-in-seydisfjordur-is-the-largest-landslide-to-have-damaged-an-urban-area-in-iceland
According
to Harpa, the landslide was of a different nature than the landslides that
occurred earlier in the week. "The preliminary observations show a
landslide scar that is up to 20 m high, and it seems to reach deep into
sediments that have not collapsed for millennia. We did not expect a landslide
of this magnitude and we underestimated conditions at the site where the
landslide fell
/about-imo/news/the-landslide-in-seydisfjordur-is-the-largest-landslide-to-have-damaged-an-urban-area-in-iceland/
wide and
1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of
the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and
landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of
the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
Of Precipitation In Latvia. XXV Nordic Hydrological conference, Northern Hydrology and its Global Role, 11-13 August, 2008, Reykjavik, Iceland. ISBN 978-9979-68-238-7. NHP Report No. 50, P. 134-142.
Hisdal, H., Barthelmie, R., Lindström, G., Kolcova, T., Kriauciuniené, J. & Reihan, A. (2007). Statistical Analysis. In: J. Fenger (Ed.) Impacts of Climate Change on Renewable Energy Sources: Their role
/ces/publications/nr/1943