79 results were found for f 홈타이▤Ø1ØX4889X4785▤黾대구수성방문아가씨梼대구수성방문안마✖대구수성빠른출장䪈대구수성숙소출장👩🏽‍🚒irresolutely.

Results:

• 51. Linnet_Ulfar_CES_2010

  HYDROPOWER IN ICELAND Impacts and adaption in future climate Authors Óli Grétar Blöndal Sveinsson (Phd) Úlfar Linnet (MSc) Elías B. Elíasson (MSc) Landsvirkjuns system •Installed power 1850 MW • 96 % Hydroelectricity • 4% Geothermal •Production capacity 13 TWh/a •Customer base • 86 % Large industries • 14 % Small businesses / Household •No connection to other countries •Reliability a major /media/ces/Linnet_Ulfar_CES_2010.pdf

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

  and Torfajo¨kull but not for Eyjafjallajo¨kull, rather than an actual sensitivity difference. Effects of cold and dry years are ignored in the uncertainty calculation. (a) (b) Using temperature at Vı´k (c) Using temperature at Hveravellir AAR (%) All seasons @bn=@T (m w. eq. yr1 8C1) Summer @bn=@T (m w.eq. yr1 8C1) All seasons @bn=@T (m w.eq. yr1 8C1) Summer @bn=@T (m w.eq. yr1 8C1) E 20
  25 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 53. Sigurður Th. Rögnvaldsson

  Veðurstofu Íslands VÍ-G99007-JA02. Sigurður Th. Rögnvaldsson 1999. Kort yfir sjálfvirkt ákvarðaðar staðsetningar jarðskjálfta á Íslandi. URL: http://hraun.vedur.is/ja/englishweb/index.html, 21.06.1999. Sigurður Th. Rögnvaldsson og R. Slunga 1993. Routine fault plane solutions for local networks: A test with synthetic data. Bull. Seism. Soc. Am. 83, pp. 1232 1247. Sigurður Th. Rögnvaldsson og R /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/

• 54. Sigurður Th. Rögnvaldsson

  Veðurstofu Íslands VÍ-G99007-JA02. Sigurður Th. Rögnvaldsson 1999. Kort yfir sjálfvirkt ákvarðaðar staðsetningar jarðskjálfta á Íslandi. URL: http://hraun.vedur.is/ja/englishweb/index.html, 21.06.1999. Sigurður Th. Rögnvaldsson og R. Slunga 1993. Routine fault plane solutions for local networks: A test with synthetic data. Bull. Seism. Soc. Am. 83, pp. 1232 1247. Sigurður Th. Rögnvaldsson og R /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur

• 55. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  tg ui da n ce fo rt ra ns bo un da ry w at er s, pr ep ar ed an d P. van der Keur et al. (floo dmanag ement )an d wat er qualit y ag re ed u po n in co m m o n u n de rs ta nd in g, creat ed th e bas is fo rth e formul atio n o f joi nt m ea su re s (Fr ijte rs an d Le en tv aa r 200 3) Mo del s (na tural ,te chnica l an d so ci al sy ste m s): Uncert aint y ha s to be incorp orated : 1: Ep ist /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 56. VI2010-006_web

  490 þar af regn 5 1 3 4 10 27 32 33 32 27 6 4 185 þar af slydda 22 14 13 12 8 1 1 1 6 21 20 16 135 þar af snjór 29 27 27 13 1 0 0 0 1 9 28 32 169 Mest á dag (mm) 31 37 41 28 31 42 20 25 25 39 28 21 42 Fjöldi regndaga 2 2 2 2 5 10 12 12 11 9 3 2 75 Fjöldi snjó/slyddud. 14 12 15 10 4 1 0 0 2 8 13 16 96 Fjöldi úrkomudaga 17 14 16 12 10 11 12 13 14 17 16 18 171 Meðalhiti (◦C) −2.2 −1.5 −1.3 1.6 5.5 9.1 /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 57. VI_2015_005

  model grid point must be taken into account. At latitude f , the grid-box size is given by dA = a2 cosf dldf ; (1) where a = 6371 km is the Earth’s mean radius, and latitude and longitude are measured in radians. For the ECMWF reanalyses, angular grid-point spacing dl = df = p=180 is constant across the domain. The low-pressure centre count at each grid point is then multiplied by dA=dA, with mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 58. VI_Arsskyrsla_2018_vef

  Nesjum 0-5 5-10 10 15 20-15 2008-2018 1979-1989 Dæmi um ólíkt rennslismynstur. 100 90 80 70 60 50 40 30 20 10 0 Júní mánaðarmeðaltal Ársmeðaltal Rennsli m 3 /s Sigurvegarinn í getraun Veðurstofunnar á Vísindavöku Rannís hlaut heimsókn á Veðurstofuna að launum. Salka Elín Sæþórsdóttir ásamt vinum sínum, Ými og Bjarti. Með þeim á myndinni er Ragnar Heiðar Þrastarson, fagstjóri landfræðilegra /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 59. VI_2015_009

  M A M J J A l ll l l l l l l l lll l l lll 0 100 200 300 60 0 80 0 100 0 Days since Sept. 1st Q (m ³/s ) vhm102 S O N D J F M A M J J A l l l ll l l l l l l l l l l l l l ll l l l l l l 0 100 200 300 30 40 50 60 70 Days since Sept. 1st Q (m ³/s ) vhm116 S O N D J F M A M J J A l l l l l l l l l l l l l l l l l l l l l l l l l l 0 100 200 300 20 0 30 0 40 0 50 0 Days since Sept. 1st Q (m ³/s /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 60. 2010_017

  an important part of the runoff from many areas. In total, approximately 20% of runoff in Iceland originates from groundwater (Hjartarson, 1994a). In the above mentioned previous simulation of runoff map for Iceland for the period 1961– 1990, groundwater was omitted. Effects of groundwater flowing across watershed boundaries were simulated by scaling the precipitation for each watershed. On watersheds /media/ces/2010_017.pdf