for abstract submissions
has been extended to 14 September. The deadline for extended abstracts is 30 October - the same day as the conference. Details about abstract submission are available via the abstract submission link.
The registration fee for the conference is 5,000 ISK (30 EUR). Students can participate in the conference at the subsidised rate of 2,500 ISK (15 EUR). The registration fee/earthquakes-and-volcanism/conferences/jsr-2009/info/
and lodging.
Registration fee: 100 USD (charged after arrival to Reykholt), including transport from Reykjavík (coordinated with flights from Europe and North America), and meals and refreshments during the meeting. The cost of hotel accommodation, 18400 IKR (~150 USD) for a single room, 21600 ISK (~170 USD) for a double room, is paid by each participant.
The registration is now closed
/lidar/lidar-2013/registration/
Plate.
The source fault of one of the earthquakes of 2000 will be visited before we cross the plate boundary back to the North America Plate.
The guide will be Professor Páll Einarsson of the University of Iceland.
The trip, departing from Reykjavík on Saturday 31 October, will last about nine hours. The estimated cost of the trip is 5000 ISK (30 EUR). This fee covers the hire of a bus
/earthquakes-and-volcanism/conferences/jsr-2009/fieldtrip/
let us know. In case of bad weather, we will find a way to drive you all to IMO and back. Wednesday 12 October 08:30 - 17:10
Seminar at Grand Hotel Reykjavík. Lunch / refreshments during
coffee breaks.17:30 - 19:30 EPOS meeting17:30 - 19:30 Those not attending EPOS can join us to Laugardalslaug Geothermal swimming pool, about 10 minutes walk from Grand Hotel. Entrance fee is around 500 ISK
/norsem/norsem2016/program/
örugt að fara fyrir Horn í um 10 sml frá landi en það yrði
að hafa góðan útvörð.
Kl.1341, kalla TFB og spyr um ETA í RVK, ETA um kl 1440.
Kl 1305, AIS umferð fyrir N- Horn. Vegna bilunnar í WS 1 var megináhersla lögð á ískönnun í
þessu flugi.
Flugskýrsla TF-SIF
12. desember 2010
Flug nr. 117410.025
Ískönnun.
Meginröndin lá um eftirtalda staði.
1. 67°47.0N 023
/media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf
Dashed lines encompass the V-shaped zone of tephra deposition. (c)
Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall
from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November.
The top portion shows its projection on an EW-vertical plane. The minimum detection height for
Grímsvötn is seen at 6 km, and the plume extends
/media/jar/myndsafn/2005EO260001.pdf
6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
1
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1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574
POLICYFORUM
combined with opera-
tions
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
list to fill
up the empty places. EUMETSAT is sending 3-5 participants representing the Baltic
countries or other member states. The number of students at the course is 20-25.
Finances
The host country is responsible for the finances and reports to EUMETSAT and its own
Economy department.
There is no course fee.
The host country covers the cost for its own participants and teachers. The host
/media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf