earthquakes in Bárðarbunga (northwestern Vatnajökull) since noon yesterday
were 4.5 in magnitude at 18:55 (24 Dec.) and at 11:02 this morning (25 Dec.). Four more
were over 4 in magnitude. In total, around 50 earthquakes were detected in Bárðarbunga. In
the dyke intrusion 9 quakes were detected, all under M2.
Now 81 km²
An overview map from Christmas Eve. The new lava is now 81 km² (80,6 km
/media/jar/Bardarbunga-2014_December-events.pdf
The hydrological simulations were performed with the Wa-
tershed Simulation and Forecasting System (WSFS) developed
and operated in the Finnish Environment Institute (Vehviläinen
et al., 2005). The WSFS is used in Finland for operational hydrolog-
ical forecasting and flood warnings (www.environment.fi/water-
forecast/), regulation planning and research purposes
(Vehviläinen and Huttunen, 1997
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
and are expressed in watts per square metre (W/m2).
5 Includes only carbon dioxide (CO2 ), methane (CH4), nitrous oxide (N2O), hydrofluorocarbons (HFCs), perfluorocarbons (PFCs) and sulphurhexafluoride(SF6), whose emissions are covered by the UNFCCC. These GHGs are weighted by their 100-year Global Warming Potentials (GWPs), using values
consistent with reporting under the UNFCCC.
6 This report
/media/loftslag/IPPC-2007-ar4_syr.pdf
to the tremor event catalog; one
tremor catalog is created per month, containing information on the tremor event ID, the start
time of the tremor, the filter triggered, and the stations triggered (see Figure 5). Each
subsequent minute, if the filter remains in a triggered state, newly triggered stations will be
appended to the existing event. Most importantly, when a tremor event is detected
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
1). Over the same period, the average total number of
people reported affected2 per decade rose by 1200%, from
approximately 38 thousand to 480 thousand. Meanwhile,
the total cost of reported damage3 doubled, from US$ 1.2
billion to US$ 2.4 billion (2006 prices), although this could
partially be explained by a higher density or vulnerability
of infrastructure and areas being used by humans. More
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
The hotel, which is located at the historic Reykholt farm, provides facilities for meetings and includes access to hot tubs and Wi Fi.
Rooms are booked by e-mail to lidar2013@vedur.is (see Registration). The cost is 18400 IKR (~150 USD) per night for a single room and 21600 ISK (~170 USD) per night for two persons in a double room (20000 ISK (~160 USD) per night for one person in a double room
/lidar/lidar-2013/accommodation/
Stóra Laxá. The combination of mild weather and intense rain is also encouraging snow to melt, which further contributes to the ongoing flood.
At 13:00 today, 26 February, the discharge of Hvítá at Fremstaver, in the northern part of the catchment, was 520 cubic metres per second. It will take floodwater in this region several hours to drain south, so maximum discharge will not be reached
/about-imo/news/nr/2660
and that the volume of the lava field is now little less than 1.4 km³. The flow of magma, during this period, was just under 100 m³ per second. The intensity of the eruption is there for slowly decreasing. Hopefully it will be possible to measure the volume of the lava field again later this week, which will give new numbers on the flow of magma.
Notes from the meeting of the Scientific Advisory
/earthquakes-and-volcanism/articles/nr/3071
and that the volume of the lava field is now little less than 1.4 km³. The flow of magma, during this period, was just under 100 m³ per second. The intensity of the eruption is there for slowly decreasing. Hopefully it will be possible to measure the volume of the lava field again later this week, which will give new numbers on the flow of magma.
Notes from the meeting of the Scientific Advisory
/earthquakes-and-volcanism/articles/nr/3071/
Jan) show, however, that the lava field has
thickened substantially during these three weeks and that the volume of the lava field is now
little less than 1.4 km³. The flow of magma, during this period, was just under 100 m³ per
second. The intensity of the eruption is there for slowly decreasing. Hopefully it will be
possible to measure the volume of the lava field again later this week, which
/media/jar/Bardarbunga-2015_January-events.pdf