84 results were found for [77AGG. COM]sm506 slot delta slot trisula 88 slot free slot 88 jp bam slot t4z.

Results:

• 51. Refsgaard_2-uncertainty

  Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec ARPEGE-CNRM ARPEGE-DMI BCM-DMI BCM-SMHI ECHAM-DMI ECHAM-ICPT ECHAM-KNMI ECHAM-SMHI Lauren P Seaby PhD project www.hyacints.dk Preliminary results Data from 8 climate models in the ENSEMBLES project (A1B) Future climate Down scaling Bias correction Global 100-250 km Scale Regional 10-25 km Hydrological 50-500 m Present climate Climate change /media/loftslag/Refsgaard_2-uncertainty.pdf

• 52. 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

• 53. VI_2020_004

  vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 54. Johannesson_Thomas_CES_2010

  The impact of climate change on glaciers and glacial runoff in the Nordic countries Tómas Jóhannesson, Guðfinna Aðalgeirsdóttir, Andreas Ahlstrøm, Liss M. Andreassen, Stein Beldring, Helgi Björnsson, Philippe Crochet, Bergur Einarsson, Hallgeir Elvehøy, Sverrir Guðmundsson, Regine Hock, Horst Machguth, Kjetil Melvold, Finnur Pálsson, Valentina Radic, Oddur Sigurðsson and Þorsteinn /media/ces/Johannesson_Thomas_CES_2010.pdf

• 55. Lawrence_Deborah_CES_2010

  areas from 3 to 15,000 km2 3 GCM/RCMs (with SRES A1B emissions) Echam5/HIRHAM5 BCM/RCA3 HadCM3Qref/HIRHAM 2 Methods for transferring RCM output to 1 x 1 km grid Delta change Empirical adjustment method (met.no) 25 calibrated hydrological models for 115 catchments Flood frequency analysis for 200-year flood ⇒ Construct pdfs from 150 results for each catchment Viksvatn (Hestadfjord) - 83.2 IS92a /media/ces/Lawrence_Deborah_CES_2010.pdf

• 56. Terms and conditions

  no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.) The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove /about-imo/the-web/conditions

• 57. Terms and conditions

  no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.) The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove /about-imo/the-web/conditions/

• 58. Protective measures

  to the "Adaptation of the Swiss Guidelines for supporting structures for Icelandic conditions (IMO Rep. 99013)" (IMO Memo TóJ-2003-05, author T. Jóhannesson) (pdf 0.03 Mb) Remarks on the design of avalanche braking mounds based on experiments in 3, 6, 9 and 34 m long chutes (IMO Int. Rep. 03024, 2003, authors T. Jóhannesson and Kr. M. Hákonardóttir) (pdf 0.8 Mb) Field observations and laboratory /avalanches/imo/protective/

• 59. Workshop on Jökulhlaup Hazards

  of over 800 inhabitants in the vicinity of the volcano. The resulting jökulhlaup drained from both the northern and southern flanks of the ice-cap, affecting an area of 57.5 and 1.5 km2, respectively. A second jökulhlaup on April 15 contained a large quantity of glacial ice; this flood propagated rapidly down the Markarfjót river, again necessitating a local evacuation. Workshop Goal The workshop /about-imo/news/nr/2251

• 60. Bardarbunga_kafli20140825

  Figure 1. The partly ice-covered Bárðarbunga volcanic system (inset, green), central volcano is indicated by capital B. Holocene lava flows from the ice-free parts of the volcanic system are shown in green, areas of thick tephra deposits are ruled. Modified after Jóhannesson and Sæmundsson (1998). No discrimination is made between lava flows of different age. In southern Iceland the area /media/jar/Bardarbunga_kafli20140825.pdf