period, and
linear trends in degrees per decade within the 2004–50 period, for the IPCC GCM
ensemble mean, the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. 23
2 Mean annual surface air temperature and total precipitation during the 1961–90
control period. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 24
3 Dependence on terrain elevation of surface air temperature
/media/ces/2010_005_.pdf
(6 106 m3) per
month for the lake below the western cauldron and 9 Gl per month for the eastern caul-
dron. Data on water accumulation and lake water composition in the western cauldron
were used to estimate the power of the underlying geothermal area as 550 MW.
For a jökulhlaup from the Western Skaftá cauldron in September 2006, the low-
ering of the ice cover overlying the subglacial lake
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
of temperature and precipitation change are
presented in map format and their interpretation is briefly discussed.
2
1. Introduction
Despite the strong scientific consensus that increases in atmospheric greenhouse gases will
lead to substantial changes in the global climate during this century (IPCC 2007), estimates of
the magnitude (and for some aspects of climate, the direction
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
to diminish. No earthquake over M3 has occurred since 21 February and none over M5 since 8 January.
GPS measurements near Vatnajökull ice cap show continuing slow deflation towards Bárðarbunga, still indicating a flow of magma from under the volcano. The subsidence of the caldera was 5 cm per day last week, correcting for the ice which slowly flows into the caldera.
An automatic gas detector
/earthquakes-and-volcanism/articles/nr/3087
to diminish. No earthquake over M3 has occurred since 21 February and none over M5 since 8 January.
GPS measurements near Vatnajökull ice cap show continuing slow deflation towards Bárðarbunga, still indicating a flow of magma from under the volcano. The subsidence of the caldera was 5 cm per day last week, correcting for the ice which slowly flows into the caldera.
An automatic gas detector
/earthquakes-and-volcanism/articles/nr/3087/
of the Scientific Advisory Board (pdf 0.4 Mb).
Seismic activity in Bárðarbunga continues to diminish. No earthquake over M3 has occurred
since 21 February and none over M5 since 8 January.
GPS measurements near Vatnajökull ice cap show continuing slow deflation towards
Bárðarbunga, still indicating a flow of magma from under the volcano. The subsidence of the
caldera was 5 cm per day last week
/media/jar/Bardarbunga-2015_February_events.pdf
: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 km² + 0,4 km²) in size. Enlarge. Institute of Earth Sciences.
24 December 2014 12:00 - from
/earthquakes-and-volcanism/articles/nr/3055
: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 km² + 0,4 km²) in size. Enlarge. Institute of Earth Sciences.
24 December 2014 12:00 - from
/earthquakes-and-volcanism/articles/nr/3055/
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
of
climate change on the energy sector are by many stakeholders considered uncertain and long-
term. Therefore, these topics may be less prioritised than other issues of more immediate (and
everyday) importance for the energy sector (such as mitigating greenhouse gas emissions,
maintenance etc.). All research was considered relevant by the “dialogue group”. The work
within the Risk Assessment
/media/ces/ces-oslo2010_proceedings.pdf