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Results:

• 51. Wind

  li.noimg { background-position : 8px 0; } Wind Wind Temperature Precipitation < day - 1 00 06 12 18 day - 2 00 06 12 18 day - 3 00 06 12 18 day - 4 /weather/forecasts/elements/south/

• 52. Wind

  li.noimg { background-position : 8px 0; } Wind Wind Temperature Precipitation < day - 1 00 06 12 18 day - 2 00 06 12 18 day - 3 00 06 12 18 day - 4 /weather/forecasts/elements/southeast/

• 53. Wind

  li.noimg { background-position : 8px 0; } Wind Wind Temperature Precipitation < day - 1 00 06 12 18 day - 2 00 06 12 18 day - 3 00 06 12 18 day - 4 /weather/forecasts/elements/west-fjords/

• 54. VI_2015_006

  on 27 July, over the glaciers, the sky was mostly cloud-free during sunshine hours, whereas on 27 July, a low-level cloud layer existed over parts of the glaciers. Comparing these two days, the shortwave radiation balance at noon over the northern part of Vatnajökull is lower by about 200 W m 2 on 27 July with overcast conditions, than on 3 August under clear skies. Differences in net shortwave /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 55. i-frame services

  The Icelandic Meteorological Office offers a service that allows web-masters to show weather information from IMO on their web-sites without effort. This service is free of charge, using the iframe technique. Two versions of iframes have been developed, one for station forecasts, text forecasts or observations, and another for weather elements (wind, temperature and precipitation forecasts /about-imo/the-web/iframes/

• 56. 47th Nordic Seismology Seminar

  and then click on "Registration" on top of that page (see screenshot). Conference costs are 30.000 ISK (~220€), to be paid upon registration. See details on cancellation policies on the registration page. Rooms at Grand Hotel Reykjavík can be booked during the registration process. Participants are free to book other potentially cheaper hotels in the vicinity.Conference costs include coffee /norsem/norsem2016/registration/

• 57. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 58. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 59. Adaptive management in relation to climate change

  to postdocs. If free places are available the course is also open to other professionals working in the subject area. Attending the course is free of charge. NONAM will provide accommodation for PhD students near the university free of charge. Participants are requested to cover travel expenses and daily allowances from their own funding. Other participants are requested to make their own /nonam/phd-summerschool/

• 60. TF-FMS_20141204_skyrsla

  on the northern site of the lava flow, minor outbreaks were observed in the southwest close to the vents and into a lava-free part in the middle of the flow, see photo on the next page. Eruption site seen from NNW, rather calm bubbling activity. Photo: Martin Hensch EBE-035-1 Eftirlitsflug /media/jar/TF-FMS_20141204_skyrsla.pdf