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Results:

• 51. VI_2009_006_tt

  vísbending um þróun farvegarins úr breiðu, óafmörkuðu rennsli yfir í skilvirkar rásir. Einnig kann að vera að í upphafi hlaupsins hafi töluvert vatnsmagn safnast upp í vatnsgeymum undir jöklinum sem ekki tóku mikinn þátt í því að flytja rennsli. v Mælingar á vatnshita í Skaftá benda til þess að hlaupvatnið sé við eða mjög nærri frostmarki þegar það kemur undan jöklinum. Þetta bendir til þess að /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 52. Hydropower - Glacier, Snow and Ice

  by remote sensing. Polar Research 2011, 7282, doi: 10.3402/polar.v30i0.7282 Guðmundsson, S., Björnsson, H., Jóhannesson, T., Aðalgeirsdóttir, G., Pálsson, F. & Sigurðsson, O. (2009). Similarities and differences in the response of two ice caps in Iceland to climate warming. Hydrology Research. 40(5), 495-502. Schuler, T. V., Crochet P., Hock R., Jackson M., Barstad I. & Jóhannesson, T. (2008 /ces/publications/nr/1940

• 53. Reykholt-abstracts

  ............................................................................................. 36 Experimental results from photon-counting laser altimetry system MABEL Henriette Skourup, René Forsberg, Sine M. Hvidegaard, Indriði Einarsson, Arne V. Olesen, Stine K. Rose, Louise S. Sørensen, Veit Helm, Stefan Hendricks, Robert Ricker, Malcolm Davidson and Tânia Casal /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 54. Warning due to violent storm

  Eiríksson Þorsteinn V. Jónsson News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 2012 2011 2010 2009 2008 2007 2006 /about-imo/news/nr/3255

• 55. VI_2014_005

  in an overall cold bias, compared with station measurements. To test, whether this is due to the HARMONIE model core or the external surface scheme, biases of 2-m temperature from SURFEX are com- pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is found that the negative temperature biases are due to shallow inversion layers near the ground, which are introduced /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 56. Adalgeirsdottir-etal-tc-5-961-2011

  ). Locations of the weather sta- tions, used to reconstruct the temperature and precipitation records, are shown with letters: Reykjavík (R), Fagurhólmýri (F), Hæll (H), Stykkishólmur (S), Teigarhorn (T), Vestamannaeyjar (V), Akureyri (A) and Hólar in Hornafjörður (HH). (B) The surface topography of Vatnajökull ice cap. Dots show the sites of mass balance and veloc- ity measurements, blue dots show /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 57. Öræfajökull : Recent research

  73–100Ásdís Helgadóttir, Emmanuel Pagneux, Matthew J. Roberts, Esther H. Jensen og Eiríkur GíslasonShort summaryChapter V. Öræfi district and Markarfljót outwash plain: Rating of flood hazards (pdf 2.35 Mb)Pages 101–122Emmanuel Pagneux og Matthew J. RobertsShort summaryChapter VI. Öræfi district and Markarfljót outwash plain: Spatio-temporal patterns in population exposure to volcanogenic floods /volcanoes/about-volcanoes/oraefajokull/new-research/

• 58. ces_SA_group_flyer_new

  are being used to analyse the occurrence of dry spells, both from historical data and from climate scenario simulations. There is significant year-to-year variability in the pattern of rainfall, and this variability is assessed based on the range of values from individual years in the analysis. No change Increase Decrease 1 9 6 1 - 1 9 9 0 1 9 3 1 - 1 9 9 0 Photo by V. Kudryavskiy, LEGMA Regional /media/ces/ces_SA_group_flyer_new.pdf

• 59. ces_flyer_glacierssnowandice

  )  Measured  1997  and  1999  ice  surfaces  of  Lang‐ jökull  and  Hofsjökull,  respectively.  c)  Steady‐state  glacier  geometries after a  few hundred year  spin‐up with  constant  mass balance forcing. Figure 3: Simulated response of Langjökull (L), Hofsjökull (H)  and southern Vatnajökull (V) to climate change. The inset  numbers are projected volumes relative to the initial stable  ice geometries /media/ces/ces_flyer_glacierssnowandice.pdf

• 60. esa_flyer_new

  EA Analyse A/S and Optensys Energianalys will forecast energy system variables, while SINTEF Energy Research will make assumptions for the energy system in different cases, include new inputs in the EMPS model and carry out simulations. Cl i ma t e Sc e nar i os G ro u p R i s ø St o c h as t i c v a r i a b l e s Clima t e s c e n a r i o NV E S M H I FE I N o r w a y S w e d e n F inla n /media/ces/esa_flyer_new.pdf