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Results:

• 31. 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

• 32. Status of unrest in Reykjanes

  August 2022 showing new dike intrusion on Reykjanes Peninsula and deformation associated with the M5.47 earthquake on 31 July 2022. Coloured fringes show ground deformation in the satellite's line-of-sight, related to the new dike intrusion beneath Fagradalsfjall which commenced on the 30th July 2022. The interferogram shows approximately 16 cm of northwestward displacement related /about-imo/news/status-of-unrest-in-reykjanes

• 33. Weather stations

  BjargtangarBreiðafjsjObs.ForecastMeteogramInfo.Obs. data BjarnareyE coastalsjObs.ForecastMeteogramInfo.Obs. data BjarnarfjarðarhálsNorth WsjInfo.Obs. data Björg í KinnNorth EsjObs.Info.Obs. data BláfeldurFaxaflsjObs.ForecastMeteogramInfo.Obs. data BláfjallaskáliFaxaflsjObs.Info.Obs. data BláfjöllFaxaflsjObs.ForecastMeteogramInfo.Obs. data BlikdalsáFaxaflsjObs.Info.Obs. data BlönduósNorth WsjObs.ForecastMeteogramInfo.Obs. data Blönduós /weather/stations/

• 34. IPPC-2007-ar4_syr

  Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf

• 35. Supporting structures stopped most of an avalanche

  of the structures is approximately at the elevation of the top row it is not clear whether the snow cover above the structure would have been released as an avalanche in the absence of the structures. In a few locations one could see that the avalanche slab had started to break up but was nevertheless moving as a more or less solid block when it was stopped by the supporting structures. It may be assumed /about-imo/news/nr/2476

• 36. Supporting structures stopped most of an avalanche

  to the west of the structures is approximately at the elevation of the top row it is not clear whether the snow cover above the structure would have been released as an avalanche in the absence of the structures. In a few locations one could see that the avalanche slab had started to break up but was nevertheless moving as a more or less solid block when it was stopped by the supporting structures. It may /avalanches/articles/nr/2475

• 37. Supporting structures stopped most of an avalanche

  ). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures. The snow cover /about-imo/news/nr/2476/

• 38. Supporting structures stopped most of an avalanche

  red curve). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures /avalanches/articles/nr/2475/

• 39. NONAM_Perrels_ea_-_From_top-down_to_integrated_economic_assessment

  From top-down to interactive economic assessments – example Finland Adriaan Perrels1, Tony Rosqvist2, Hanna Virta1 1. Finnish Meteorological Institute FMI; 2. Technical Research Centre of Finland VTT email address: adriaan.perrels@fmi.fi Finland started to assess possible economic impacts of climate change as part of the so-called SILMU program1 from 1992 to 1995. In that time it was still /media/loftslag/NONAM_Perrels_ea_-_From_top-down_to_integrated_economic_assessment.pdf

• 40. Avalanche bulletin - Eyjafjörður (experimental)

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/inner_eyjafjordur