72 results were found for 杏彩国际娱乐2平台【┃稳定２17⒋31┃扣】】.

Results:

• 51. The August glacial outburst - one of the larger jökulhlaups to have affected Skaftá in recent decades

  the interval between floods is short the flood tends to be smaller, with the eastern cauldron responsible for the largest floods.Accurate early warning to the public, based on innovative GPS measurements in the cauldronThe beginning of the August jökulhlaup was registered by continuous GPS measurements of the ice-shelf over the eastern cauldron. These measurements showed a slight lowering early on 31 /about-imo/news/the-august-glacial-outburst-one-of-the-larger-jokulhlaups-to-have-affected-skafta-in-recent-decades

• 52. Dataseries and components

  ), quantity (mm), pH Heavy metals in aerosol: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/m3) Cl, NO3-N, SO4-S (µg/m3) Hg (pg/m3) Persistent organic pollutants (POPs), same for precipitation (ng/l) and air (pg/m3): alfa-HCH, beta-HCH, gamma-HCH p,p'-DDE p,p'-DDD o,p'-DDT p,p'-DDT dieldrin HCB cis-chlordan, trans-chlordan, trans-nonachlor, PCB-28, -31, -52, -101, -105, -118, -138, -153, -156 /pollution-and-radiation/pollution/components/

• 53. On the Bárðarbunga gradual caldera collapse

  volcano collapsed during the eruption as 1.9 km³ of magma flowed laterally from a magma reservoir under the volcano. About one quarter formed a 48 km long dyke (0.5 km³) while about three quarters were erupted in Holuhraun (1.4 km³) over the six months between 31 August 2014 and 27 February 2015. The subsidence bowl formed in Bárðarbunga was up to 65 m deep and the area where subsidence exceeded 1 m /about-imo/news/on-the-bardarbunga-gradual-caldera-collapse/

• 54. Future Climate and Renewable Energy - Impacts, Risks and Adaptation 31 May - 2 June Presentations

  Publications and presentations Future Climate and Renewable Energy - Impacts, Risks and Adaptation 31 May - 2 June Presentations /ces/publications/nr/2016

• 55. Isskyrsla_20100407

  Ísskýsla 7.apríl Flug 03410.025 Miðvikudaginn 7 apríl var farið í ískönnunarflug á TF-SIF úti fyrir vestfjörðum. Kl.1115 var komið að ísröndini sem lá til NA um eftirtalda staði: 1. N65°50'- W028°05' 2. N65°44' -W027°49 ' 3. N65°56'- W027°08' 4. N66°12' -W026°21' 5. N66°31'- W025°57' 6. N66°43'- W025°49' 7. N66°40'- W025°24' 8. N67°05'- W024°32' 9. N67°14' -W023°56' 10.N67°19'- W023°32' 11.N67°40 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 56. VI_2015_007

  1 Introduction ................................................................................................ 7 2 Study area and data ..................................................................................... 7 2.1 River basins .......................................................................................... 7 2.2 Streamflow data /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 57. Keranen_Jaana_CES_2010

  Case study – Using the CES risk assessment framework in the biomass and wind power sectors Conference on Future Climate and Renewable Energy: Impacts, Risks and Adaptation 31 May – 2 June 2010 Oslo, Norway Jaana Keränen VTT Technical Research Centre of Finland 202/07/2010 Outline square4 Background information square4 Risk Assessment Framework (RAF) square4 Case-studies: biomass & wind power /media/ces/Keranen_Jaana_CES_2010.pdf

• 58. Reports and publications

  2,9 2006 PREPARED - third periodic report February 1, 2005 - July 31, 2005 (PDF) Ragnar Stefánsson et al. (32 authors) 132 9,6 2006 PREPARED - final report (PDF) Ragnar Stefánsson 66 8,6 2006 PREPARED - Management and resource usage summary Months 25-30: February 1 - July 31, 2005 (PDF) Ragnar Stefánsson, Barði Þorkelsson 18 1,5 2006 Tjörnes fracture zone. New and old /earthquakes-and-volcanism/reports-and-publications/

• 59. VI_2015_006

  energy fluxes on 27 July 2012......................................... 31 15 Average downward energy fluxes on 27 July 2012 over the ocean ..................... 32 16 Average downward energy fluxes on 3 August 2012 ...................................... 34 17 Average downward energy fluxes on 3 September 2012 .................................. 35 18 Relative humidity at 2 mAGL /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 60. VI_2015_009

  4 Contents 1 Introduction ................................................................................................ 7 2 Study area and data ..................................................................................... 7 2.1 River basins .......................................................................................... 7 2.2 Streamflow data /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf