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• 31. Safetravel

  has supported the Safetravel project since its beginning in 2010. ICE-SAR's office leads the project with the help of many SAR team members as well as others with thorough experience in travelling in Iceland in different conditions. Safetravel is supported by a number of sponsoring companies. SOS Iceland app The newest option is SOS Iceland, an app which is easy to use. It can be used /about-imo/news/nr/2497

• 32. Safetravel

  project since its beginning in 2010. ICE-SAR's office leads the project with the help of many SAR team members as well as others with thorough experience in travelling in Iceland in different conditions. Safetravel is supported by a number of sponsoring companies. 112 Iceland app An option is 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs /about-imo/news/nr/2707

• 33. Safetravel

  -SAR's office leads the project with the help of many SAR team members as well as others with thorough experience in travelling in Iceland in different conditions. Safetravel is supported by a number of sponsoring companies. 112 Iceland app An option is 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs or if someone is lost. Tourist can also leave /about-imo/news/nr/2878

• 34. Safetravel in winter

  night and day, all year round. 112 Iceland app Safetravel provides 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs or if someone is lost. Tourist can also leave their "trail" in case of search. From Safetravel's web-site, the app can be downloaded for either Android phones, Windows phones or iPhone: First of all you can call for help by pressing /about-imo/news/nr/3220

• 35. 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

• 36. VI_2019_009

  To distinguish between rain and snow, the volume is com- pared to the water equivalent but the volume of snow is ten times larger. Figure 1. How PWD22 determines the type of precipitation. Using the information about the changes of the backscatter signal, water equivalent and temper- ature the Vaisala Present Weather Detector can give information about the type of precipitation. It is also used /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 37. 2013_001_Nawri_et_al

  /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 38. VI_2015_006

  ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 39. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 40. Machguth_Horst_CES_2010

  experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf