73 results were found for 【┋添加扣217⒋31〓】杏彩彩票3d平台.

Results:

• 31. The final CES conference, 31 May-2 June 2010

  Climate and Energy Systems - CES The final CES conference, 31 May-2 June 2010 7.9.2010 /ces/nr/1979

• 32. The flood in Múlakvísl has subsided

  News Rafleiðni í Múlakvísl 29.-31. júlí 2017 /about-imo/news/the-flood-in-mulakvisl-has-subsided

• 33. Publications 2020

  Barsotti, Sigrún Karlsdóttir, Anna María Ágústsdóttir, Björn Oddsson, Íris Marelsdóttir, Þorvaldur Þórðarson, Þórólfur Guðnason & Bogi B. Björnsson 121 31 /about-imo/publications/2020/

• 34. News

  News © Veðurstofa Íslands Vatnshæð, hiti og rafleiðni í Gígjukvísl frá kl. 14:00 31. október til kl. um 09:00 1 /about-imo/news/bigimg/2039

• 35. Conference proceedings Oslo 31 May - 2 June 2010

  Publications and presentations Conference proceedings Oslo 31 May - 2 June 2010 Future Climate and Renewable Energy /ces/publications/nr/1966

• 36. Information Management

  relevance of the CES project. In Proc. of Future climate and renewable energy: Impacts, risks and adaptation, Oslo, 31 May - 2 June 2010. Partners CICERO, Center for Klimaforskning, Norway Denmark Meteorological Institute Ea /ces/publications/nr/2127

• 37. The Climate and Energy Systems project final conference

  conference 10.9.2010 The final conference of the CES project "Future Climate and Renewable Energy - Impacts, Risks and Adaptation" was held in Oslo from 31 May to 2 June. The conference was organised around five themes: Past and present changes in climate /about-imo/news/nr/1983

• 38. VI_2014_006

  .................................................................................................. 56 Appendix I Observed versus deterministic temperature forecasts over the period 01/09/2001– 31/08/2006. .................................................................................................. 59 Appendix II Observed versus deterministic precipitation forecasts over the period 01/09/2001– 31/08/2006 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 39. VI_2020_004

  ....................................................................................................................... 31 4.1 General approach ...................................................................................................... 31 4.2 Numerical model ....................................................................................................... 32 4.2.1 Plume rise model ............................................................................................. 33 4.2.2 VOL /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 40. Grímsvötn 2010

  On October 31, a glacier outburst flood (jökulhlaup*) emerged from beneath the Skeiðarárjökull glacier, a southern outlet of the Vatnajökull ice cap. The floodwaters originate in the subglacial lake Grímsvötn, 50 km upstream from the glacier margin. The lake has been a source of such floods for centuries, but the size of the floods has varied greatly. The present flood is small and no threat to roads /hydrology/articles/nr/2040