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98 results were found for 에이루트매수▣WWW༝S77༝KR▣濫에이루트무상증자抷에이루트분석譗에이루트실적ѷ🍷elevation/.


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  • 61. Dyrrdal_Anita_CES_2010

    • Analyse future snow scenarios Introduction Data & Methods Results 0 50 100 150 200 250 300 350 400 450 0-100 100- 200 200- 300 300- 400 400- 500 500- 600 600- 700 700- 800 800- 900 900- 1000 1000- 1100 1100- 1200 1200- 1300 1300- 1400 1400- 1500 1500- 1600 1600- 1700 1700- 1800 1800- 1900 1900- 2000 2000- 2100 2100- 2200 Høyde (m o.h.) A n t a l l v æ r s t a s j o n e r Elevation of met.no /media/ces/Dyrrdal_Anita_CES_2010.pdf
  • 62. 2010_016

    subcatchments vhm 167 and vhm 269) and the non-glacier covered watershed Sandá í Þistilfirði vhm 26. ................................................................................................................. 9 Figure 2. Elevation distribution for Sandá í Þistilfirði (vhm 26, blue curve) and Austari- Jökulsá (vhm 144, red broken curve /media/ces/2010_016.pdf
  • 63. 2010_017

    .................................................................................................................. 10 Figure 4. Elevation distribution for Sandá í Þistilfirði (vhm 26, blue curve) and Austari- Jökulsá (vhm 144, red broken curve). .................................................................................... 16 Figure 5. Comparison of mean yearly temperature 1961–2005 for Sandá í Þistilfirði (vhm 26); an interpolation /media/ces/2010_017.pdf
  • 64. VI_arsskyrsla2020

  • 65. ces_geus_paakitsoq_full_report

    was derived from observations in the area of Swiss Camp (h is the surface elevation in m a.s.l): τcl = 1.0 − 0.78n 2 exp(−0.00085h) (3) 3.2 Validation Procedure Implemented in the mass balance model is the comparison of the RCM-data (= the model input) to observations from weather stations on the ground. The observations are compared to the values of the RCM grid-cells they are located in. Before /media/ces/ces_geus_paakitsoq_full_report.pdf
  • 66. 2005EO260001

    caldera covered by 150- to 250-m-thick ice (Figure 1). Its highest peak, Grímsfjall, on the southern caldera rim, reaches an elevation of 1722 m. Volcanic eruptions there, numbering several per century, are phreatomagmatic because of the ice cover, and they usually persist for days to weeks. Geothermal activity continu- ously melts the overlying ice, and meltwater accumulates in a subglacial /media/jar/myndsafn/2005EO260001.pdf
  • 67. Paper-Olafur-Rognvaldsson_91

    of validation data. COMPARISON WITH GLACIOLOGICAL DATA The spatial variability of the mass balance on large ice masses, such as Vatnajökull and Langjökull ice caps, can be mapped given data along several profiles extending over the elevation range of the ice caps. Mass balance has been observed on parts of Vatnajökull ice cap in SE-Iceland since 1991 (Björns- son et al., 1998) and from 1996 /media/ces/Paper-Olafur-Rognvaldsson_91.pdf
  • 68. VI_2015_006

    elevation contour lines are drawn at 1000 mASL, indicating roughly the extent of the glaciers. 15 3 Radiation fluxes at the surface With increasing time past the summer solstice (20 June 2012), the solar energy per unit area received at the Earth’s surface, for the same cloud and snow conditions, decreases due to the shorter days and lower sun altitude angles. The characteristics of the solar cycle /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
  • 69. Monitoring of Hekla

    -grained ash could be lofted to high elevation, with international implications for air travel. Since 1970, the volcano has erupted at roughly decadal intervals (1970, 1980-81, 1991 and 2000). This is one reason why the volcano is now considered to be ‘overdue', as the last eruption occurred more than 16 years ago. Before 1970, Hekla erupted less frequently, with repose intervals up to 120 years /about-imo/news/monitoring-hekla
  • 70. Hofsjökull ice cap gains mass

    to the retreat of the ice cap since then. The yellow lines delineate the catchments of glacial rivers fed by the ice-cap. The river names are given in blue but the names of the ice-flow basins in black. Spring measurements The winter balance was measured during a ten day expedition in early May. The winter snow thickness was unusually high (Fig. 2) and above 1400 m elevation snow thicknesses /about-imo/news/nr/3229

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