Holuhraun lava field
Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather and visibility, shows the outlines of the new lava in exceptionally high detail (see full image) as they were two days ago. Referral: (c) DLR/ Fjarkönnun ehf./IsViews 10/2014.
9 October
/earthquakes-and-volcanism/articles/nr/3011
the following five parameters
were adjusted: (1) Storage coefficient of direct runoff kd; (2) 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/media/ces/2010_016.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
earthquakes were observed in the dike intrusion and about 20 close to
Herðubreið.
The eruption can not be seen on the webcams.
9 October 2014 - a high definition image of the lava
Holuhraun lava field
Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which
Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather
and visibility, shows
/media/jar/Bardarbunga-2014_October-events.pdf
Holuhraun lava field
Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather and visibility, shows the outlines of the new lava in exceptionally high detail (see full image) as they were two days ago. Referral: (c) DLR/ Fjarkönnun ehf./IsViews 10/2014.
9 October
/earthquakes-and-volcanism/articles/nr/3011/
from the glacier margins). This
was done by shifting the x and y coordinates of the
40 m40 m DEMs in 5 m steps and calculating the
correlation to the corresponding values of the 5 m5 m
EMISAR DEM. In all cases, both the maximum correla-
tion and minimum standard deviation yielded the same
shift. After the co-registration, the same ice-free areas
were used to correct the vertical offset of the DMA
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf