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


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  • 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 hhmmss.ms 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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