4 occurred at the caldera, an M4.6 at 17:34 yesterday and an M4.3 at 05:48 this morning, as well as a few over 3 in size. A dozen earthquakes were detected in the dike, all small.
26 October 2014 12:00 - from geoscientist on duty
Approximately 80 earthquakes have been detected around the Bárðarbunga caldera. The strongest events were M5.3 today at 05:48 on the southeastern caldera rim and M4.7
/earthquakes-and-volcanism/articles/nr/3011
hours.
The largest occurred at 01:05 this morning, M5.3 at the southwestern rim. Two quakes over 4
occurred at the caldera, an M4.6 at 17:34 yesterday and an M4.3 at 05:48 this morning, as
well as a few over 3 in size. A dozen earthquakes were detected in the dike, all small.
26 October 2014 12:00 - from geoscientist on duty
Approximately 80 earthquakes have been detected around the Bárðarbunga
/media/jar/Bardarbunga-2014_October-events.pdf
4 occurred at the caldera, an M4.6 at 17:34 yesterday and an M4.3 at 05:48 this morning, as well as a few over 3 in size. A dozen earthquakes were detected in the dike, all small.
26 October 2014 12:00 - from geoscientist on duty
Approximately 80 earthquakes have been detected around the Bárðarbunga caldera. The strongest events were M5.3 today at 05:48 on the southeastern caldera rim and M4.7
/earthquakes-and-volcanism/articles/nr/3011/
113,1
84,2
193
182
Keflavíkurflugvöllur
1219,5
109,4
117,9
35,0
274
199
The
annual total in Reykjavík was 1054.9 mm, 28 percent above the 1971
to 2000 mean. In
Akureyri the total was 695.9 mm, 34 percent above the 1971 and 2000
mean. This is the third highest annual sum in Akureyri since the
beginning of registration in 1928 (it was higher
2014 and 1989
/about-imo/news/the-weather-in-iceland-in-2018
method with
MLE.
34
Figure 18 – 1M5 map based on 24-hour accumulated precipitation, with projections
from the RCP 8.5 for the interval 2080 – 2100, using the 90th percentile from the climate
model ensemble. Results obtained using the Peak-over-Threshold method with MLE.
35
5.2.3.2 1M5 results for the hydropower catchments
Table 8 shows the median 1M5 results for all the catchments
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
J. Bufton, J. Dezio, D. Hancock, H. Harding, T. Herring, B. Minster, K. Quinn, S.
Palm, J. Spinhirne, and R. Thomas. 2002. “ICESat’s laser measurements of polar ice, atmosphere, ocean, and land,” J. Geodyn., 34(3).
We acknowledge the support of the National Power Company of Iceland, the Public Roads Administration, the Research Fund of
Iceland (Rannís), the University Research Fund
/media/ces/glacier_mass_balance_poster.pdf
(Percent) By
Year Built Categories
Percent of Homes Damaged By Year Built
Categories
36
24
26
28
30
32
34
Pre 1980 80-96 97-2002 Post 2002
Percent Damaged
All Homes – Damage Per Square
Foot
All Homes - Damage Per Square Foot
2
2.5
D
a
m
a
g
e
P
e
r
S
q
.
F
o
o
t
0
0.5
1
1.5
< 120 120-129 130-139 140-149 > 149
D
a
m
a
g
e
P
e
r
S
q
.
F
o
o
t
Pre 1980
1980-1996
1997-2002
Post 2002
/media/loftslag/FMI_-_Disaster_Mitigation.pdf
Nature 438,
303 (2005).
8. J. Lu, G. A. Vecchi, T. Reichler, Geophys. Res. Lett. 34,
L06805 (2007).
9. S. Manabe, R. J. Stouffer, J. Geophys. Res. 85, 5529
(1980).
10. P. S. Eagleson, in Scientific Basis of Water-Resource
Management (National Academy Press, Washington, DC,
1982).
11. N. C. Matalas, in Global Change and Water Resources
Management (Water Resources Update No. 112,
Universities
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf