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West fjords - earthquakes during the last 48 hours (Preliminary results)
Map
Table
Earthquake location 01 May 12:55 GMT
Time and magnitude of earthquake 01 May 12:55 GMT
/earthquakes-and-volcanism/earthquakes/westfjords/
BIEG 13:44 13:44 01:0101:05 240
BIEG 13:44 13:55 BIRK 16:59 17:01 03:04 03:17 606
00:00 00:00 0
00:00 00:00 0
00:00 00:00 0
00:00 00:00 0
Samtals 04:05 04:22 846
Flugleið:
Flugskýrsla TF-SIF
11. Janúar 2012
Flug nr. 00212.025
Kl.1520, ískönnun hefst á radar N- af Horni.
N- og NV- af Straumnesi er talsverð nýmyndun. Næst landi var nýmyndunin um 11,5 sml.
NNV- af
/media/2012/isskyrsla_2012-01-11.pdf
SizeTimeQualityLocation
1.001.05 09:20:04Check.3.1 km E of Flatey
1.301.05 07:22:42Check.8.3 km SW of Grímsfjall
1.101.05 07:09:37Check.12.3 km E of Grímsey
1.001.05 06:51:46Check.36.1 km W of Grímsey
1.001.05 05:43:14Check.4.4 km W of Dreki
1.001.05 05:05:16Check.10.2 km E of Hekla
1.801.05 04:36:18Check.6.4 km ESE of Bárðarbunga
1.701.05 01:52:56Check.10.9 km NNE
/m/earthquakes/latest
cluster north of Bárðarbunga that was active during the first days
automatic automatically detected events in the whole country, number of events outside the
Vatnajökull are comparably small in number, contains also false detections.
A safe number is “around 23.000-25.000 events”.
checked manually checked events
document created on 01. October 2014 at 18:15
/media/jar/event_numbers_07102014_1800.pdf
of
low frequency tremor suggestive of volcanic activity.
Earthquakes: Three earthquakes ranging in size from magnitude 0.9 to 1.2 have been
detected beneath Grímsvötn today.
GPS deformation: No change; see status report from 01 November 2010.
Overall assessment: Tremor levels at seismic station 'grf' have reduced slightly in the last
24 hours. Discharge measurements in the Gígja river show
/media/vatnafar/flod/Grimsvotn_status_2010-11-05_IES_IMO.pdf
An analysis of simulated and observed storm
characteristics
- Can we expect a change in the future?
R.E. Benestad, CES, June 01 2010
Number of cyclones:
RCM
analysis
CCI
(Benestad & Chen, 2006) righttoleftmark
No change in storm frequency?
RCM:
N corresponds
|v| too high
...or simulated wind speeds?
•CCI
•triangulation
Method: storm characteristics
RCM: storms too small
too strong.
Gradient
/media/ces/Benestad_Rasmus_CES_2010.pdf
ECONOMIC EFFECTS OF CLIMATE CHANGE ON THE TOURISM SECTOR
IN SPAIN
By
Ana Gargallo-Castel
Department of Business Administration
University of Zaragoza, C/ Ciudad Escolar, s/n
44003 TERUEL, SPAIN
Phone: 00 34 978 61 81 01. Fax 00 34 978 61 81 03
Email: gargallo@unizar.es
Luisa Esteban-Salvador
Department of Finance and Accounting
University of Zaragoza, C/ Ciudad Escolar, s/n
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf