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• 51. ice-chart_colour-code-standard

  -250-130 FY thin ice (white ice) first stage 2.5.1.1 175-250-000 FY thin ice (white ice) second stage 2.5.1.2 000-200-020 FY medium ice 2.5.2 000-120-000 FY thick ice 2.5.3 180-100-050 Old ice 2.6 255-120-010 Second-year ice 2.6.1 200-000-000 Multi-year ice 2.6.2 150-150-150 Fast ice of unspecified SoD 2.6 210-210-210 Ice shelf 10.3 255-255-255 Ice of undefined SoD - 255-255-255 Drifting ice of land /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 52. Hare_2-participation

  .. … … … … … … [1] Ehemals: Gute fachliche Praxis Expert Stakeholders Computer model All stakeholders - Discussions based on Group model Forum 1 15.9.04 Forum 2 3.11.04 Forum 3 12.04.05 Forum 5 07.09.05 Forum 4 15.06.05 Multi-Criteria Eval. Testing Solutions Interviews Jan/Feb 05 10 Reporting: Cooperative Writing Accepted Short Discussion neue Formulierung Accepted Definition of Aims & Contents /media/loftslag/Hare_2-participation.pdf

• 53. Re-evaluation needed of the size of the hazard area

  05.04 at 15:40Photos of two new volcanic fissures near to the initial eruption site in Geldingadalir, located approximately 700 meters NE of the craters in Geldingadalir. The new fissures are in total 200 meters long. The lava from the fissures is non viscous and flows fast in a narrow lava-river into Meradalir valley, east of the new fissures, where a new lava field is forming. Photos: Björn /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir

• 54. Reykholt-abstracts

  ....................................................................................... 16 Mass balance and volume changes of Eyjafjallajökull ice cap, from 1984 to 2010, deduced by multi-temporal elevation maps Victoria H. Hamilton Morris ................................................................................................. 17 Construction and analysis of lidar mosaics of sea ice floe /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 55. Journal_of_Hydrology_Veijalainen_etal

  annual temperature varied from 5 C to 2 C and precipitation from 450 mm to 700 mm (Drebs et al., 2002). Finland is a long country and the temperature gradient is strong especially in winter (Fig. 1a), which affects the accumula- tion and melting of snow. In south-western Finland the thermal winter lasts on average for 100 days whereas in northern Finland this season is about 100 days longer /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 56. VI_2014_006

  0 0 20 12 % Grassland <1 43 25 10 25 % Woodland <1 0 0 2 2 % Moss 59 25 0 14 13 % Little or no vegetation 35 27 30 63 36 % Wetland 0 5 46 6 7 % Lakes 6 <1 <1 <1 3 300 400 500 600 700 800 30 0 40 0 50 0 60 0 70 0 km km 2400 2200 2000 1800 1600 1400 1200 1000 800 600 400 200 0 m.a.s.l Watershed Glacier vhm19 vhm10 vhm26 vhm64 vhm66 Figure 1. Topography of Iceland and location of the watersheds /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 57. raisanen_ruosteenoja_CES_D2.2

  are available. In practice, this correction is more important for precipitation than temperature forecasts (Ruokolainen and Räisänen 2007). Another underlying assumption in the method is that the probability distribution of climate changes depends only on the simulated multi-model mean global mean warming. This assumption is not exactly valid, but analysis of model simulation suggests /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 58. Early work and an overview of measurements

  Nansen both wrote interesting papers on the subject after Thoroddsen died. Their conclusions were similar to Thoroddsen's. These supported the work of the Danish scientist Speerschneider, the compiler of sources on ice off the coast of Denmark from AD 700 onwards. He concluded that no significant long-term changes had occured during this period. Thoroddsen did exchange views with the differently /climatology/articles/nr/1138

• 59. Early work and an overview of measurements

  Nansen both wrote interesting papers on the subject after Thoroddsen died. Their conclusions were similar to Thoroddsen's. These supported the work of the Danish scientist Speerschneider, the compiler of sources on ice off the coast of Denmark from AD 700 onwards. He concluded that no significant long-term changes had occured during this period. Thoroddsen did exchange views with the differently /climatology/articles/nr/1138/

• 60. Kok_et_al._TFSC_published_2011

  of EC-funded projects. This paper reports on activities that took place within the SCENES project (www.environment. /syke/scenes), which set out to undertake a multi-dimensional multi-scale scenario process, with a strong foundation in science and broad participation of stakeholders. This should provide new ideas about managing the future of water in Europe. Scenarios were developed at three scales /media/loftslag/Kok_et_al._TFSC_published_2011.pdf