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
years, IMO has participated in extensive research supported by the European Commission, EC, and various other funds, which is meant to improve this situation. The results of the collective research were published in 2009 in a book called The design of avalanche protection dams - Recent practical and theoretical developments.
The design of protective measures in the run-out zones of avalanches
/about-imo/news/nr/1631
possibly pooling in hollows and lows in the landscape, e.g. in Hrunagil and Hvannárgil gullies. Civil Protection Department is on the alert.
Over the last few days the air temperatures at Fimmvörðuháls, 900-1100 m above sea level, have been from -6°C down to -14°C with strong northeasterly winds and gusts over 20 m/s; in these circumstances wind chill can be considerable. For weather outlook, please
/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
an 80 km2 ice-filled
caldera. The characteristic activity is explosive basaltic eruptions occurring on central volcano flanks or the
fissure swarm. Known eruptions have mostly been VEI 3-4 but occasionally VEI 5-6 (bulk volume of tephra up
to 10 km3). The largest eruptions occurred in the early Holocene, effusive basaltic eruptions on the fissure swarm
with lava volumes ≥20 km3. Eruption
/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
Research Basins (NRB) International Symposium and Workshop: 12 August - 18 August, 2009, Iqaluit-Pangnirtung-Kuujjuaq : [conference proceedings, field guide] /editors: Kathy L. Young, William Quinton.Toronto: York University, August 2009. bls. 285-289.
Snorrason, Á. & Harðardóttir, J. (2008). Climate and Energy Systems (CES) 2007-2010. A new Nordic energy research project. In O. G. B. Sveinsson, S. M
/ces/publications/nr/1936
Eruption in Eyjafjallajökull
Status Report: 11:00 GMT, 7 June 2010
Icelandic Meteorological Office and Institute of Earth Sciences, University
of Iceland
Compiled by: Gunnar B. Guðmundsson, Sigurlaug Hjaltadóttir, Ármann Höskuldsson,
Björn Sævar Einarsson, Haraldur Eiríksson, Þorvaldur Þórðarsson, Guðrún
Larsen, Sigrún Hreinsdóttir and Bergthóra S. Thorbjarnardóttir.
Based on: IMO seismic
/media/jar/Eyjafjallajokull_status_2010-06-07_IES_IMO.pdf