it
is then very difficult to anticipate how the situation will evolve. The
inflation is continuing at present (3. Sept 2021) and will be closely monitored
by IMO which will distribute additional information in case of further changes. More information about Askja volcano is available at icelandicvolcanos.is Data from the GPS station
OLAC (location shown in the InSAR image), for the North
/about-imo/news/uplift-signal-detected-in-askja-volcano
2015, 2025, 2035 and 2050
North (Blanda) East (Karahnjukar) South (Thorisvatn)
Change in average inflow to the main storage reservoirs
Watershed
A
v
e
r
a
g
e
i
n
f
l
o
w
[
m
3
/
s
]
0
2
0
4
0
6
0
8
0
1
0
0
1
2
0
Last 50 years
Last 20 years
Last 15 years
Last 10 years
Last 5 years
Temperature corrected
Transformation of climate measurements
•Change in temperature
• 0.75 °C/100y 1950-1975
• 1.55
/media/ces/Linnet_Ulfar_CES_2010.pdf
no glow was seen in a flight 27 Feb.
Volcanic gas can still get dispersed all over the country, see a note from meteorologist on duty; emission of gases has not ended, neither from the inactive vents nor the extensive lava field. See how toxic values may actually get higher.
The lava field is 85 km². Its average thickness is 10 - 14 m (max 40 m) and its volume is 1.4 km³. The maximum subsidence
/about-imo/news/nr/3097
The current period of unrest began in July 2011, when a short-lived glacial flood burst from Mýrdalsjökull in connection with increased seismicity. Since then, several hundred micro-earthquakes have taken place within the area of the caldera. The enclosed graph shows how the ongoing activity compares to earlier episodes of seismic unrest at Katla in 1999 and 2002-2004.
In the early hours
/about-imo/news/nr/2360
BIOMATH, Ghent University, Gent, Belgium
d Water Quality Modelling modelEAU, University Laval, Quebec, Canada
Received 20 December 2005; received in revised form 5 February 2007; accepted 7 February 2007
Available online 27 April 2007
Abstract
A terminology and typology of uncertainty is presented together with a framework for the modelling process, its interaction with the broader
water
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
and in the
national radio.
Information and any questions on air pollution can be sent to The Environment Agency through the email
gos@ust.is. The Environment Agency is especially looking for information from people who have been in
contact with high concentrations of gas; where they were, at what time it happened, how the gas cloud
looked (colour and thickness of the cloud) and how they were affected
/media/jar/Factsheet_Bardarbunga_20141027.pdf
been in
contact with high concentrations of gas; where they were, at what time it happened, how the gas cloud
looked (colour and thickness of the cloud) and how they were affected by it.
Three scenarios are considered most likely:
The eruption on Holuhraun declines gradually and subsidence of the Bardarbunga caldera stops.
Large-scale subsidence of the caldera occurs, prolonging
/media/jar/Factsheet_Bardarbunga_20141029.pdf
about 42 meters.
Energy of the geothermal areas in Bardarbunga is now few hundred megawatts and the melting of water is
estimated around 2 cubic meters per. second. The water goes into Skjálfandafljót og Jökulsá á Fjöllum. The flow is
too small to effect the total water flow of the rivers.
Around 20 smaller earthquakes are detected in the dyke and at the eruption site in Holuhraun, all
/media/jar/Factsheet_Bardarbunga_20141031.pdf