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• 41. Instructions on using Atlantic Ocean forecasts

  of the wind direction. Wind-speed is symbolised by diagonal lines at the end of the barb; a long line represents 5 m/s, a short line 2.5 m/s and a triangle represents 25 m/s. Temperature forecast: Temperature levels are shown over the Atlantic Ocean in degrees Celsius (°C) at an altitude of about 1,500 m above the ocean surface. This altitude equates to an air pressure of 850 hPa /weather/articles/nr/1218

• 42. VI_2015_007

  to conduct the flood frequency analysis and develop the index flood method. Figure 2 presents the time of occurrence of AMF for each catchment. One can see that for most catchments, the AMF is mainly observed between July and November, i.e mainly caused by heavy rainfall, rather than spring snowmelt. 2.3 Meteorological data Gridded daily air temperature at 2 m above ground (Crochet & Jóhannesson /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 43. Jökulhlaup in Skaftá - progress

  the area covered by the gauge. The discharge at Eldvatn near Ásar peaked around 13:00 showing discharge of approximately 2200 m³/s. The area outside the main water channel will be flooded for coming days. Gas measurements Two SO2 sensors and one MultiGas have been installed in order to monitor the gas released from the glacial outburst occurring along the Skaftá river. The sensors have been /about-imo/news/nr/3211

• 44. CES_D2.4_solar_CMIP3

  the A1B scenario. In the panels for winter and autumn, contour interval is 25 MJ m−2, in those for spring and summer 50 MJ m−2. The colour scale is the same in all panels. Fig. A5. The absolute insolation change under the A2 scenario. 11 Fig. A6. The absolute insolation change under the B1 scenario. 12 (B) TIME SERIES Fig. A7 shows the time series of seasonal changes in incident radiation /media/ces/CES_D2.4_solar_CMIP3.pdf

• 45. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  are currently melting at a fast rate. Over recent decades, annual mass balance field observations on the three largest ice caps in Iceland* Langjo¨kull (ca. 900 km2), Hofsjo¨kull (ca. 890 km2) and Vatnajo¨kull (ca. 8100 km2)*show a declining specific mass balance from about 0 m yr1 w. eq. on average from 1980 to 1994 to 1 to 1.3 m yr1 w. eq. on average after 1995 (Bjo¨rnsson et al. 2002 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 46. norsem_lindholm

  Neotectonics in Nordland; NEONOR 2 C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf, M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners The Nordland shore region is known to be seismically active with deep local sediment basins on the continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland have /media/norsem/norsem_lindholm.pdf

• 47. glacier_mass_balance_poster

  - accuracy on cm scale at gentle sloping terrain - higher errors at rough and steep sloping terrain - often false values due to frequent occurence of clouds in the area c) GPS profiles and points observed at ice free areas - accuracy ~1 m in elevation Characteristics Ice cap E: Eyjafjallajökull To: Torfajökull Ti: Tindfjallajökull Area (km2) Range in elevation (m a.s.l.) 81 15 14 180-1630 660-1480 /media/ces/glacier_mass_balance_poster.pdf

• 48. norsem_dori

  Holuhraun eruption was accompanied by over 70 5.7>M>5 earthquakes on the rim of the Bárðarbunga caldera. A GPS station was installed in the ice- filled caldera and captured both the slow subsidence of the caldera and displacement seismograms at 20 Hz of many of the larger collapse earthquakes. The GPS seismograms add constraints in the interpretation of the caldera collapse /media/norsem/norsem_dori.pdf

• 49. Hock_Regine_CES_2010rs

  Projections -50% -48%-73% -78% -80% +3% Storglaciären Mårmaglaciären Scandinavia Comparison with all other glacier regions Volume reduction and sea-level equivalent (SLE) until 2100 for 19 glacier regions Radic and Hock, submitted Antarctica Sub-Antarctic Islands Greenland New Zealand South America II South America I Iceland Arctic Canada West Canada and West US Alaska High Mountain Asia North /media/ces/Hock_Regine_CES_2010rs.pdf

• 50. Group-1_Scenarios-for-AWM

  t / c o s t ratio H i g h L o w S c enar i o 1 S c ena r io 2 Present time 20302020 Socio E c onomic D e v elopme n t Figure 1. Scenario building for AWM in Horsens Fjord To estimate of the adaptation strategy (Table 2) we will use back-casting approach. The assessments of the productivity of this approach are based on main big strategies which need to have an attention. One of them /media/loftslag/Group-1_Scenarios-for-AWM.pdf