túlkun á línu VIII á Nesjavöllum. Skýrsla Orkustofnunar OS-87024/JHD-15 B. Orkustofnun, Reykjavík.
Sigurður Th. Rögnvaldsson 1992. Fault plane solutions by combined use of polarities and body wave amplitudes. Fil. lic. ritgerð við Uppsala Háskóla, ISSN 1170 7320.
Sigurður Th. Rögnvaldsson 1994. Microearthquakes in South Iceland: Fault plane solutions and relative locations. Doktorsritgerð við
/earthquakes-and-volcanism/conferences/jsr-2009/sigurdur
contains a list of stations that have been off-line for at least two weeks in the spring
of 2011.
Table 3. Off-line stations.
Station ID Station name Category Problem
BALD Búrfellsalda við
Kárahnjúka
A Receiver is not logging. Needs to be reset
ENTA Enta B No data from University of Iceland
FITC Fitjarás B Data link down since 12-04-2011
HAUC Háumýrar B Poor radio link
HVEL Hveravellir B/media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
coordinates) and other places you plan to visit
Few words about the equipment
Plan B
Travellers can leave their travel plan with ICE-SAR, provided it includes a contact or relative whose responsibility is to alert ICE-SAR if the travellers do not arrive at the right time. ICE-SAR also provides a more extensive service with trip monitoring as an option within the travel plan.
The web-page
/about-imo/news/nr/2878
you plan to visit
Few words about the equipment
Plan B
Travellers can leave their travel plan with ICE-SAR, provided it includes a contact or relative whose responsibility is to alert ICE-SAR if the travellers do not arrive at the right time. ICE-SAR also provides a more extensive service with trip monitoring as an option within the travel plan.
Further information
A personal location beacon
/about-imo/news/nr/3220
be ordered at the EU Bookshop and it can be accessed on the web both as PDF suitable for the screen (1.5 Mb) and in higher resolution suitable for printing (27.9 Mb).
Edited by T. Jóhannesson of the Icelandic Meteorological Office and by P. Gauer, P. Issler and K. Lied of the Norwegian Geotechnical Institute. Contributions by M. Barbolini, U. Domaas, T. Faug, P. Gauer, K. M. Hákonardóttir, C. B/about-imo/news/nr/1631
Below are various photos from Fimmvörðuháls, taken over the last few days.
Einar Kjartansson, 27th March 2010:
Ólafur Sigurjónsson, 25th March 2010:
Árni Sigurðsson, 24th March 2010:
Árni Sigurðsson, 24th March 2010:
Árni Sigurðsson, 24th March 2010:
Gunnar B. Guðmundsson, 24th March 2010:
Einar Kjartansson, 22th March 2010:
See photographer and date above each photo
/about-imo/news/nr/1858
Information about the UK Met Office can be found at http://www.metoffice.gov.uk/
Interested students should contact
For more information, please e-mail Sara (sara@vedur.is) and Throstur (ThrosturTh@hi.is).
The application must include the following
1. A cover letter including a. Your name.
b. Academic status – please note the admission requirements.
c. Contact details.
d. The names
/media/frettir/AdMSstudent_May2017_.pdf
Figure 1. The partly ice-covered Bárðarbunga volcanic system (inset, green), central volcano is indicated by
capital B. Holocene lava flows from the ice-free parts of the volcanic system are shown in green, areas of thick
tephra deposits are ruled. Modified after Jóhannesson and Sæmundsson (1998). No discrimination is made
between lava flows of different age. In southern Iceland the area
/media/jar/Bardarbunga_kafli20140825.pdf
to a slight inaccuracy in the calculations. The figure on the right loosely shows the relationship between m/s and a few Beaufort-values.
The prerequisites of the calculations above are:
The equation: W = 0.836B3/2 where W is windspeed in m/s and B is value on the Beaufort-scale.
1 m/s = 3.6 km/h = 1.944 knots (2.237 miles per hour)
Below is a detailed table with comparison between Beaufort
/weather/articles/nr/1283