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• 31. FAQ

  meters-size (bombs and ballistics) can land up to few km from the vent and can represent a serious hazard in the proximity of a volcano. Those particles that decouple quickly from the volcanic plume due to their size and weight fall close to the volcano and constitute the proximal deposit. Smaller particles can reach higher altitudes and persist in the atmosphere for days and weeks /volcanoes/grimsvotn-activity/faq/

• 32. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley

• 33. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley/

• 34. GA_2009_91A_4_Andreassen

  ) and summer balance (bs) have been carried out at Storbreen since 1949. Here we apply a simple mass balance model to study the climate sensitivity and to reconstruct the mass balance series prior to 1949. The model is calibrated and validated with data from an automatic weather station (AWS) operating in the ablation zone of Storbreen since 2001. Re- gression analysis revealed that bw was best mod /media/ces/GA_2009_91A_4_Andreassen.pdf

• 35. askja_minnisblad_ens

  Minnisblað ___________________________________________________ 7 Figure 8. Right: An areal photo of the rockslide area in Suðurbotnar. There is evidence of older movement which is probably an old rockslide. Left: The outline of the rockslide. The lake shore has retreated in places (yellow areas), the displacement being up to 50 m. Around the middle of the deposit /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 36. CES_D2.4_solar_CMIP3

  (an average of 18 mod- els) is depicted in Figs. 3 (in percentage terms) and 4 (in absolute terms). In the relative sense, largest changes occur in winter in central Scandinavia and southern Finland, where more than 5% of incident radiation would be lost (Fig. 3(a)). According to the t test, the signal is statistically significant at the 1% level. Over the Barents Sea, the decline is even larger /media/ces/CES_D2.4_solar_CMIP3.pdf

• 37. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 38. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  : The outline of the rockslide. The lake shore has retreated in places (yellow areas), the displacement being up to 50 m. Around the middle of the deposit, the edge seems to have advanced (purple area). Background: Loftmyndir ehf. Analyses: Ásta Rut Hjartardóttir and Þorsteinn Sæmundsson. Fig. 9 Figure 9. Geological map showing the outline of the rockslide, as well as eruptive fissures /avalanches/articles/nr/2929

• 39. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  s fro m climat e ch ang e an d cr o ss bou ndar y adaptatio n measu res . In th e Netherl and s fo r hyd rodyna m ic mod el syst em s lik e SOB EK- W AQ UA (loca lleve l) an d e.g . fo rR hi ne flo w (ba sin wi de )c o n sid er ab le u n ce rta in tie s ex ist (W ee rts et al .200 3) D ev el op m en to fi nt eg ra te d ba sin m o de l( flo od ing an d poll ution) . 2: St at ist ic al /q ua lit /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 40. 2010_005_

  Coupl. Glob. Clim. Mod., Canadian Centre for Climate Modelling and Analysis, Victoria CSIRO MK 3.5 Glob. Clim. Mod., Commonwealth Scient. and Industrial Res. Organisation, Australia MIROC 3.2 Medres Model for Interdiscip. Res. on Clim., Division of Climate System Research, Tokyo, Japan MIUB Echo G Coupled Circulation Model, Meteorological Institute of the University of Bonn, Germany MPI ECHAM5-r3 /media/ces/2010_005_.pdf