82 results were found for l 파생상품거래〔WWW-BYB-PW〕 파생상품매매 파생상품투자파생상품리딩㏯액토즈소프트 iRm.

Results:

• 51. VI_2009_006_tt

  farvegarins undir jöklinum út frá rúmmáli vatns sem þar hefur safnast fyrir benda til þess að viðnám gegn vatnsrennsli við jökul- botn minnki eftir því sem líður á hlaupið. Undir lok hlaupsins runnu á bilinu 80– 90 m3 s 1 um farveg sem var einungis einn þriðji hluti af rúmmáli farvegar sem flutti svipað vatnsmagn á fyrsta eða öðrum degi eftir að hlaupið hófst við jökuljaðar. Þessi niðurstaða er /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 52. Paper-Olafur-Rognvaldsson_91

  The role of orography was found to be crucial in determining the precipitation dis- tribution and amount. Atmospheric flow over Iceland was simulated for the period January 1961 through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale model (Grell et al., 1995). The domain used is 123× 95 points, centered at 64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 53. IPPC-2007-ar4_syr

  of significant changes consistent with warming Percentage of significant changes consistent with warming 89%94%100% 100% 100% 100% 100% 100% 99%100%98% 96% 91% 94% 94% 90%90%92%94% 355 455 53 119 NAM LA EUR AFR AS ANZ PR* TER MFW** GLO 5 2 106 8 6 1 85 7650 120 24 7645 28,115 28,586 28,671 Changes in physical and biological systems and surface temperature 1970-2004 33 Topic 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf

• 54. Protective measures

  developments (European Commission, Directorate-General for Research, Publication EUR 23339, 2009, ISBN 978-92-79-08885-8, ISSN 1018-5593, DOI 10.2777/12871. Edited by T. Jóhannesson, P. Gauer, P. Issler and K. Lied. Contributions by M. Barbolini, U. Domaas, T. Faug, P. Gauer, K. M. Hákonardóttir, C. B. Harbitz, D. Issler, T. Jóhannesson, K. Lied, M. Naaim, F. Naaim-Bouvet and L. Rammer) (pdf 1.6 Mb; high /avalanches/imo/protective/

• 55. The design of avalanche protection dams

  years, IMO has participated in extensive research supported by the European Commission, EC, and various other funds, which is meant to improve this situation. The results of the collective research were published in 2009 in a book called The design of avalanche protection dams - Recent practical and theoretical developments. The design of protective measures in the run-out zones of avalanches /about-imo/news/nr/1631

• 56. General about the project

  Research Basins (NRB) International Symposium and Workshop: 12 August - 18 August, 2009, Iqaluit-Pangnirtung-Kuujjuaq : [conference proceedings, field guide] /editors: Kathy L. Young, William Quinton.Toronto: York University, August 2009. bls. 285-289. Snorrason, Á. & Harðardóttir, J. (2008). Climate and Energy Systems (CES) 2007-2010. A new Nordic energy research project. In O. G. B. Sveinsson, S. M /ces/publications/nr/1936

• 57. Bio Energy

  The International Forestry Review 12(5), p 28. Alam, A., Kilpeläinen, A. and Kellomäki, S. (2010). Forest biomass for energy production ? Potentials, management and risks under climate change. Conference on Future Climate and Renewable Energy: Impacts, Risks and Adaptation, 31.5. ? 2.6.2010, Oslo, Norway. Conference Proceedings pp. 50-51. Kellomäki, S. (2007). In: J. Fenger (Ed.) Impacts of Climate Change /ces/publications/nr/1939

• 58. norsem_korja

  ), most of the earthquakes (80%) occur in the upper crust down to 17 km in depth, a minority (19%) in the middle crust (17-31 km) and only a few in the lower crust 31-45 km (1%) [1]. The seismogenic layer is less than 30 km in depth. The layer seems to be rather uniform across Fennoscandia. We suggest that the middle to lower crustal boundary may add compositional and rheological constraints /media/norsem/norsem_korja.pdf

• 59. New article on glacier changes in

  cubic kilometers of water), or a total of 540 ± 130 Gt. This corresponds to 16 ± 4% of the volume of the glaciers around 1890. About half of this mass was lost from 1994 to 2019 or 240 ± 20 Gt, which is about 9.6 ± 0.8 Gt / year on average during that period. Vatnajökull has thinned by 45 m on average in the period 1890–2019, Langjökull by 66 m and Hofsjökull by 56 m. This corresponds /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years

• 60. ces_flyer_glacierssnowandice

  )  Measured  1997  and  1999  ice  surfaces  of  Lang‐ jökull  and  Hofsjökull,  respectively.  c)  Steady‐state  glacier  geometries after a  few hundred year  spin‐up with  constant  mass balance forcing. Figure 3: Simulated response of Langjökull (L), Hofsjökull (H)  and southern Vatnajökull (V) to climate change. The inset  numbers are projected volumes relative to the initial stable  ice geometries /media/ces/ces_flyer_glacierssnowandice.pdf