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• 41. Avalanche bulletin - Eyjafjörður (experimental)

  .a tspan, .sa-active .text .sa tspan, .s-active .text .s tspan, .sv-active .text .sv tspan, .v-active .text .v tspan, .nv-active .text .nv tspan { fill: #1F4E78; font-size: 120%; font-weight: 700; font-size: 120%; } /* Staða */ .status { /* width: 267px; height: 249px; */ width: 80px; height: 74px; } .status .arrow { fill: #6d8fae; display: none; } .status .indic /avalanches/forecast/inner_eyjafjordur

• 42. Avalanche bulletin - Tröllaskagi

  .a tspan, .sa-active .text .sa tspan, .s-active .text .s tspan, .sv-active .text .sv tspan, .v-active .text .v tspan, .nv-active .text .nv tspan { fill: #1F4E78; font-size: 120%; font-weight: 700; font-size: 120%; } /* Staða */ .status { /* width: 267px; height: 249px; */ width: 80px; height: 74px; } .status .arrow { fill: #6d8fae; display: none; } .status .indic /avalanches/forecast/trollaskagi

• 43. 100 years since Katla erupted

  and it includes a 9 by 14 km caldera, with ice-thickness up to 700 m.Historical eruptions of Katla are predominantly explosive, generating ash-rich plumes and glacial outburst floods (jökulhlaups). In historical times, jökulhlaups have inundated Mýrdalssandur, to the east. Prehistoric jökulhlaups are also known to have drained to the west and north-west of the volcano, affecting Markarfljót.Lava /about-imo/news/100-years-since-katla-erupted

• 44. Avalanche bulletin - Eyjafjörður (experimental)

  .a tspan, .sa-active .text .sa tspan, .s-active .text .s tspan, .sv-active .text .sv tspan, .v-active .text .v tspan, .nv-active .text .nv tspan { fill: #1F4E78; font-size: 120%; font-weight: 700; font-size: 120%; } /* Staða */ .status { /* width: 267px; height: 249px; */ width: 80px; height: 74px; } .status .arrow { fill: #6d8fae; display: none; } .status .indic /avalanches/forecast/inner_eyjafjordur/

• 45. Avalanche bulletin - Tröllaskagi

  .a tspan, .sa-active .text .sa tspan, .s-active .text .s tspan, .sv-active .text .sv tspan, .v-active .text .v tspan, .nv-active .text .nv tspan { fill: #1F4E78; font-size: 120%; font-weight: 700; font-size: 120%; } /* Staða */ .status { /* width: 267px; height: 249px; */ width: 80px; height: 74px; } .status .arrow { fill: #6d8fae; display: none; } .status .indic /avalanches/forecast/trollaskagi/

• 46. VI_arsskyrsla2020

  the Icelandic Met O?e has transformed into a multi-hazard monitoring and research institute of national and international importance. The innovative work of the Icelandic Met O?e in the twentieth century continues today through sustained advancements in knowledge and technology. ÁRSSKÝRSLA 2019 8 Frumkvæði frá verkalýðshreyfingunni vegna öryggis sjómanna Í kjölfar mikilla sjóslysa árið 1916 benda /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 47. Joining forces in weather forecasting and climate research

  Ireland's weather service, goes under the name of United Weather Centres West (UWC-West). This is part of a broader collaboration between ten national weather services in Europe, known as United Weather Centres (UWC), which plan to operate a common multi-national weather forecasting system by the end of the decade. “This collaboration has a long history and specially the collaboration between /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 48. RaisanenJouni_CES_2010

  of winter mean temperature in Helsinki: 1961-2008 vs. 2010 Only best (multi-model average) estimates are shown here Shift to right: mild winters more common, cold winters less common Narrower distribution with a higher peak: a slight decrease in variability, i.e., largest warming of coldest winters -12 4 Note: probability ~ area How frequently at least as mild as in winter 2007-08 (+1.3°C)? 1961 /media/ces/RaisanenJouni_CES_2010.pdf

• 49. Program

  terrestrial lidar to understand the mechanisms driving melt pond evolution on sea ice in the Canadian Arctic Hans-Gerd Maas and Ellen Schwalbe, TU Dresden, Institute of Photogrammetry and Remote Sensing, Germany. 3D velocity fields at Jacobshavn Isbrae glacier from multi-temporal terrestrial laser scanner data Lunch 12:30–13:30 Thursday, 13:30–15:00 ‒ Process studies – II Kjetil Melvold and Thomas /lidar/lidar-2013/program/

• 50. Moellenkampetal_etal-2010

  Coad 5, Jean-Emmanuel Rougier 6, Matthew Hare 7, Natalie A. Jones 8, Albena Popova 4, Dominique Rollin 3, Pascal Perez 9,10, and Stewart Burn 11 ABSTRACT. Broad-scale, multi-governance level, participatory water management processes intended to aid collective decision making and learning are rarely initiated, designed, implemented, and managed by one person. These processes mostly emerge from /media/loftslag/Moellenkampetal_etal-2010.pdf