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in Askja
8 Projects
9 The weather in Iceland 2014
10 Finance
11 Sta?publications
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
3
One of the main goals of the merger of the Hydrological Service,
HS, and the Icelandic Meteorological Office, IMO, was to improve
the capabilities regarding monitoring, warnings and emergency
response due to natural hazards. Prior
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
bursts of
seismic tremor (1–3 Hz), and later becoming
periodic with energy between 2 and 8 Hz. After
18 October, seismicity increased to three events
per day (Figure 2b). Synchronous with this
increase, the ISGPS station SKRO (Figure 1b)
moved 9 mm westward over the following eight
days, and returned to its original position on 1
November (Figure 2c), suggesting subsurface
magma movement
/media/jar/myndsafn/2005EO260001.pdf
a systematic com-
parison of results to observed precipitation has been carried out. Un-
dercatchment of solid precipitation is dealt with by looking only at
days when precipitation is presumably liquid or by considering the
occurrence and non-occurrence of precipitation. Away from non-
resolved orography, the long term means (months, years) of observed
and simulated precipitation are often
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
An overview of past and future surveys of Iceland conducted by the NERC ARSF
Eric Lutz, Bob Hawley, Michelle Hofton, John Sonntag, Kelly Brunt and Roseanne Dominguez, Department of Earth Sciences, Dartmouth College, USA. Validation of NASA laser altimeters at Summit, Greenland
Finnur Pálsson, Eyjólfur Magnússon, Sverrir Guðmundsson, Helgi Björnsson, Hannes H. Haraldsson, and Tómas Jóhannesson
/lidar/lidar-2013/program/
be broader than stated? (7) Further
elicit and specify the distribution (shape and percentiles or
characterising parameters). (8) Verify with the expert that
the distribution that you constructed from the expert’s re-
sponses correctly represents the expert’s beliefs. (9) Decide
whether or not to aggregate the distributions elicited from dif-
ferent experts (this only makes sense if the experts
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
activity is in the dyke and at similar depth as before (8-12km). One earthquake of M5 occurred at 08:13 AM by the northern rim of the Bardarbunga caldera. Two minutes earlier (08:11) another event of M3.9 occurred at a similar location. A few earthquakes were detected near Askja, the biggest one of M2.7.
Dyngjujökull - flight today
The edge Dyngjujökull by Holuhraun, view to the north. Note
/earthquakes-and-volcanism/articles/nr/3000
18:14 - from geoscientist on duty
Since midnight over 1100 earthquakes have been detected by the automatic system. The dyke
does not appear to have migrated further north since noon. The main activity is in the dyke
and at similar depth as before (8-12km). One earthquake of M5 occurred at 08:13 AM by the
northern rim of the Bardarbunga caldera. Two minutes earlier (08:11) another event
/media/jar/Bardarbunga-2014_August-events.pdf
activity is in the dyke and at similar depth as before (8-12km). One earthquake of M5 occurred at 08:13 AM by the northern rim of the Bardarbunga caldera. Two minutes earlier (08:11) another event of M3.9 occurred at a similar location. A few earthquakes were detected near Askja, the biggest one of M2.7.
Dyngjujökull - flight today
The edge Dyngjujökull by Holuhraun, view to the north. Note
/earthquakes-and-volcanism/articles/nr/3000/
regimes of
Number of flood and drought disasters in the past
decades per case study
0
2
4
6
8
10
12
1977-1986 1987-1996 1997-2006
Time period
Total number of flood and
drought disaster
s
Rivierenland
Alentejo
Upper Tisza - Hungary
Upper Tisza - Ukraine
Fig. 1 Number of reported flood and drought disasters in the past
decades in Rivierenland, Alentejo, Hungarian part of Upper Tisza,
and Ukrainian
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf