81 results were found for 【K06.CC】领英linkedin真人1000好友出售 wsjkh.

Results:

• 61. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 62. NONAM_1st_workshop_summary_v3

  -out group, assuming the initiative is at the public side. Red: inside transport system; blue: direct impact on size & quality of demand for road vehicle movements; grey: auxiliary services that strongly interact with effects of CC. Various possible effects of climate change on road infrastructure and its users The expected effects of a changing climate in Nordic countries imply among others /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

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

  ; (1) where N is the number of years between the elevation maps, A1 is the average area (m2) of the ice cap over N years, r is the scaling factor from the density of ice (900 kg m3) to water (1000 kg m3), DV D ¯hA2; (2) is the total volume loss (m3), D ¯h is the N year area- average elevation change (m) for the whole ice cap and A2 is the maximum area (m2) of the ice cap. In this study we use /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 64. Bárðarbunga 2015 - February events

  Sciences, 17 - 19 February: There is only one active vent inside the crater and the surface of the molten lava continues to sink. The lava channel has crusted over, except the 200 - 300 m nearest to the vent. The eruption column reaches no more than 1000 m above ground. The photos below show breakouts 15 – 16 km ENE of the vent, fed by the closed lava pathway which is inflating the lava field /earthquakes-and-volcanism/articles/nr/3087

• 65. Bárðarbunga 2015 - February events

  Sciences, 17 - 19 February: There is only one active vent inside the crater and the surface of the molten lava continues to sink. The lava channel has crusted over, except the 200 - 300 m nearest to the vent. The eruption column reaches no more than 1000 m above ground. The photos below show breakouts 15 – 16 km ENE of the vent, fed by the closed lava pathway which is inflating the lava field /earthquakes-and-volcanism/articles/nr/3087/

• 66. Bardarbunga-2015_February_events

  report from the eruption site Excerpt from a new field report from the Institute of Earth Sciences, 17 - 19 February: There is only one active vent inside the crater and the surface of the molten lava continues to sink. The lava channel has crusted over, except the 200 - 300 m nearest to the vent. The eruption column reaches no more than 1000 m above ground. The photos below show breakouts 15 /media/jar/Bardarbunga-2015_February_events.pdf

• 67. IMO_AnnualReport2014

  Percolating water from the melt- ing snow may have increased the rate of movement. Seismic data indicate that a sudden movement occurred around 40 minutes be- fore the slide, but at 23:24 the failure point was reached and the rockslide was released. ? Width of fracture line: 800 m ? Vertical drop: 350 m ? Run-out length beyond the lake shore: ~1000 m ? Volume: ~30–50 million m³ ? Estimated /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 68. Journal_of_Hydrology_Veijalainen_etal

  for flood discharge analysis are located near the flood inundation analysis sites. The four sites for flood inundation analysis were selected from areas where major flood damages have occurred and which are listed as flood prone areas by Timonen et al. (2003). The national flood hazard mapping with 20–1000 year floods, based on ob- served and extrapolated flood discharges, was also carried out /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 69. Refsgaard_2-uncertainty

  precipitation • Delta change (monthly correction factors to observed precipitation) • Direct method – Histogram Equalisation Method (Gamma function correction of RCM simulated precipitation) Statistical downscaling of precipitation - Delta change versus Direct method 0 1000 2000 3000 4000 5000 6000 0 0. 1- 1 1- 3 3- 5 5- 7 7- 10 10 -1 5 15 -2 0 20 -2 5 25 -3 0 30 -3 5 35 -4 0 40 -4 5 45 -5 0 50 -5 5 55 /media/loftslag/Refsgaard_2-uncertainty.pdf

• 70. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf