on the respective day. Poster presentations (during all three coffee breaks) Tuesday 11 October Arrival and
check-in. Most flights will arrive in the afternoon, so you should be
at your hotel around 17:00/18:00.19:00 Kickoff
party at IMO (Bústaðavegur 7, 108 Reykjavík). We will meet you at 18:30 outside Grand Hotel and walk together to IMO. Should anybody prefer to get a lift by car, please
/norsem/norsem2016/program/
to give an oral or poster presentation, whether you intend to participate in the excursion to Langjökull on Friday afternoon, and whether you arrive on June 19 or 20. A block booking of rooms has been made at the Reykholt hotel. Potential participants are encouraged to register early due to limited number of hotel rooms.
The deadline for registration was: April 15 – abstract, registration
/lidar/lidar-2013/registration/
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
a headliner to wear under the helmet and snow scooter gloves.
The excursion starts at 14:00 on Friday afternoon (departure by bus from the hotel at Reykholt). The snow scooter trip is from ~15:00 to ~17:00. The bus will drive the participants back to the hotel and departs to Reykjavík at ~18:00
/lidar/lidar-2013/excursions/
who want to stay not too far from the city centre at a reasonable price. Participants flying from Iceland on Saturday may want to stay in a hotel in Keflavik to be close to the airport in the morning since many flights leave early in the morning, in particular flights to Europe. Hotels in and near Keflavík are listed here. The closest hotel is just by the airport (Airport Hotel Smári).
The map
/lidar/lidar-2013/travel-info/
run, and the blended initial field for the subsequent run. During the
first forecast hour, model simulations tend towards the values at the end of the previous run, but
especially in the interior of the island, some significant differences remain.
14
For 2-m air temperature and 10-m wind speed, this is illustrated in Figure 5, based on average
diurnal cycles, calculated separately for grid points
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf