89 results were found for V 신용카드현금화 〔TKTAKA1-CՕM〕 티켓타카 W 신용카드현금화 전문 포탈 핸드티켓⛳denunciator/.


  • 21. Avalanche bulletin - Northern Westfjords

    /* Áttaviti */ .attaviti { /* width: 277px; height: 300px; */ width: 80px; height: 95px; } .directions .n, .directions .na, .directions .a, .directions .sa, .directions .s, .directions .sv, .directions .v, .directions .nv { fill: #BDD7EE; } .n-active /avalanches/forecast/northern_westfjords/
  • 22. Avalanche bulletin - Southwest corner

    /* Áttaviti */ .attaviti { /* width: 277px; height: 300px; */ width: 80px; height: 95px; } .directions .n, .directions .na, .directions .a, .directions .sa, .directions .s, .directions .sv, .directions .v, .directions .nv { fill: #BDD7EE; } .n-active /avalanches/forecast/southwest_corner/
  • 23. Avalanche bulletin - Tröllaskagi

    /* Áttaviti */ .attaviti { /* width: 277px; height: 300px; */ width: 80px; height: 95px; } .directions .n, .directions .na, .directions .a, .directions .sa, .directions .s, .directions .sv, .directions .v, .directions .nv { fill: #BDD7EE; } .n-active /avalanches/forecast/trollaskagi/
  • 24. Sea ice in August 2009

    in the period 6th to the 22nd, eight from ships and one from land. The icebergs were closest to land at 66°28,81'N og 21°23,86'V and close to Selsker (66°07,5N og 21°31'V). No seaice was in the Greenland Strait in August and northeasterly winds prevailed in the area /sea-ice/monthly/2009/nr/2330
  • 25. Recent publications

    Oddur Sigurðsson, Óðinn Þórarinsson, Philippe Crochet, Tómas Jóhannesson & Þorsteinn Þorsteinsson (2012). Floods in Iceland. In: Z. W. Kundzewicz (ed), Changes in Flood Risk in Europe. Oxfordshire: IAHS Special Publication 10, 257-276. Hálfdán Ágústsson & Haraldur Ólafsson (2012). The bimodal downslope windstorms at Kvisker. Meteorology and Atmospheric Physics 116(1-2), 27-42, doi:10.1007/s00703 /about-imo/arctic/completed-projects/publications/
  • 26. VI2010-006_web

  • 27. VI_2009_012

    ; the revised Mw value. Last two columns show the respective distance coefficients, describing the decay of PGV and PGA. Events written in bold letters are from Table 1. yyyymmdd Lat.(°N) Lon.(°W) Depth MLw(M0SIL) MLw(v) Mw(M0SIL) Mw(v) a(v) a(a) 20071120 184854.3 63.949 20.989 1.84 3.3 3.9 3.0 3.5 -1.7 -2.0 19990720 060402.1 63.904 22.027 5.37 3.5 3.5 3.1 3.1 -1.7 -2.2 19990525 180305.2 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 28. ces-glacier-scaling-memo2009-01

    2008) together with a regression line through this data set and a regression line derived for a data set of more than a hundred valley glaciers (Bahr and others, 1997). The regression lines are of the form v = csg ; (5) where v and s are glacier volume and area, respectively. The coefficient and exponent for the Icelandic ice caps are c = 0:048, g = 1:23, when the area and volume are expressed /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 29. VI_2017_009

    2005 until 2100 and select two periods as a focus of this study; the mid-century (2041-2060) and the late-century (2081-2100). Furthermore, we choose RCP4.5 and RCP8.5 as emission scenarios. The numbers 4.5 and 8.5 indicated the possible radiative forcing in W/m2 in the year 2100 compared to pre- industrial values, and are a measure of the strength of the anthropogenic greenhouse effect /media/vedurstofan-utgafa-2017/VI_2017_009.pdf
  • 30. glacier_mass_balance_poster

    the two periods: from -0.2 to 0.2 m yr-1 w. eq. during first period 1979/1984-1998 to -1.8 to -1.5 m yr-1 w. eq. for the more recent period 1998 to 2004. This declining mass balance takes place at the same time as the average regional temperatures increased by ~1 °C from the first to the second period (1980-1998 to 1998 to 2004). Location Data Eyjafjallajökull (E), Tindfjallajökull (Ti /media/ces/glacier_mass_balance_poster.pdf

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