83 results were found for f 동구키스방┥［dm080.com］✥동구건마 동구주점 동구출장 동구휴게텔❄동구휴게텔.

Results:

• 31. High resolution precipitation maps for Iceland

  maps for 1971-2000 Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson. Reference: Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model /weather/articles/nr/1625

• 32. Isskyrsla_20100120

  Flugskýrsla TF-SIF Dags 20.01.2010. Flug nr. 00410.025 Áhöfn: Flugstjóri: Benóny Ásgrímsson Flugmaður: Hafsteinn Heiðarsson Yfirstýrimaður: Auðunn F. Kristinsson Stýrimaður: Guðmundur E. Sigurðsson Stýrimaður: Vilhjálmur Ó. Valsson Aðrir: Earl Wilson Flugtími: Flugvöllur Hreyfing Flugtak Flugvöllur Lending Stöðvað Flugtími Blokktími Sjml. BIRK 18:45 18:50 BIRK ########### ########### 720 00:00 00 /media/hafis/skyrslur_lhg/Isskyrsla_20100120.pdf

• 33. norsem_lindholm

  Neotectonics in Nordland; NEONOR 2 C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf, M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners The Nordland shore region is known to be seismically active with deep local sediment basins on the continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland have /media/norsem/norsem_lindholm.pdf

• 34. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 35. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 36. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 37. Kok_1-scenarios-lecture-1

  scale: The Hierarchy Theory • Emerged as part of a movement toward a general science of complexity • Rooted in various other disciplines but operationalised by ecologists in the 1970s and 1980s • Key references: Allen, T. F. H. and T. B. Starr. 1982. Hierarchy: perspectives for ecological complexity. University Chicago Press. Allen T. F. H. and T. Hoekstra. 1992. Toward a unified ecology /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 38. 2010_005_

  which are significantly lower com- pared with similar beginning and end years. Consequently, for the 2004–50 period, the average RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are somewhat larger than for the reduced IPCC ensemble mean. Additionally, the tabulated values of SAT differences between the 1961–90 control period and either the 2021–50 /media/ces/2010_005_.pdf

• 39. Isskyrsla_20101212

  Flugskýrsla TF-SIF 12. desember 2010 Flug nr. 117410.025 Áhöfn: Flugstjóri Hafsteinn Heiðarsson Flugmaður Jakob Ólafsson Flugmaður 2 / Þjálfunarfl. Yfirstýrimaður Auðunn F. Kristinsson Stýrimaður Gunnar Örn Arnarson Stýrimaður Stýrimaður Aðrir 9 farþegar, 4 til Akureyrar en 5 með allt flugið. Flugtími: Flugvöllur Hreyfing Flugtak Flugvöllur Lending /media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf

• 40. hafisskyrsla_18ag2011

  Flugskýrsla TF-SIF 18. ÁGÚST 2011 Flug nr. 10611.025 Áhöfn: Flugstjóri Hafsteinn Heiðarsson Flugmaður Kristín Viktorsdóttir Observer Yfirstýrimaður Auðunn F. Kristinsson Stýrimaður Gunnar Örn Arnarson Stýrimaður Stýrimaður Aðrir Garðar Árnason Flugtími: Flugvöllur Hreyfing Flugtak Flugvöllur Lending Stöðvað Flugtími Blokktími Sjml. BIRK 10:10 10:13 BIRK /media/hafis/skyrslur_lhg/hafisskyrsla_18ag2011.pdf