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83 results were found for Con JZMOR, la frode non ha scampo: proteggi i tuoi investimenti.


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  • 31. 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
  • 32. VI_2014_001

    ...................................................................................... 31 7 References .................................................................................................. 32 Appendix I - Daily Index flood models for Region 1. .......................................... 35 Appendix II - Daily Index flood models for Region 2. ........................................ 36 Appendix III - Comparison between /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
  • 33. Kok_et_al._TFSC_published_2011

    This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites /media/loftslag/Kok_et_al._TFSC_published_2011.pdf
  • 34. Eriksson_Garvill_Nordlund_2006

    were collected through a mail survey in Sweden, Acceptability of travel demand managemen of problem awareness, persona Louise Erikssona,b,, Jo¨rgen Garvil aDepartment of Psychology bTransportation Research Unit Available onlin Abstract y 26 (2006) 15–26 t measures: The importance norm, freedom, and fairness la,b, Annika M. Nordlunda,b a˚ University, Sweden Umea˚ University, Sweden 14 July 2006 /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
  • 35. Guidelines2-for-rapporteurs

    ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf
  • 36. CES_BioFuels_Flyer_new

    ) and changing climate (CC:CC) 1. Current climate (CU) - varying thinning regimes (0%, 15%, 30%,45%) 2. Changing climate (CC) - varying thinning regimes (0%, 15%, 30%,45%) 3. Current (CU) & changing climate (CC) - current thinning regime 4. Current (CU) & changing climate (CC) - changed thinning regimes C l i m a t e s c e n a r i o s M ea s u r e m en t s o f c l i m a t e p /media/ces/CES_BioFuels_Flyer_new.pdf
  • 37. Moellenkampetal_etal-2010

    Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Daniell, K. A., I. White, N. Ferrand, I. S. Ribarova, P. Coad, J.-E. Rougier, M. Hare, N. A. Jones, A. Popova, D. Rollin, P. Perez, and S. Burn. 2010. Co-engineering participatory water management processes: theory and insights from Australian and Bulgarian interventions. Ecology and Society 15(4): 11 /media/loftslag/Moellenkampetal_etal-2010.pdf
  • 38. VI_2009_006_tt

    sem reiknaður þrýstingur í hlaupfarveginum var ekki trúverðugur. Þetta bendir til þess að fræðilegur grundvöllur líkansins sé ófullnægjandi til þess að skýra hraðvaxandi jökulhlaup. vi Acknowledgments First I want to thank my supervisor, Tómas Jóhannesson, for his superb guidance on all stages of this work, from initial planning to final read-through and from tempera- ture recorder calibration /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 39. IMO at the Arctic Circle Assembly 2017

    than 50 countries. The Arctic Circle has in recent years grown into a large and influential forum for international dialogue and cooperation on the future of the Arctic. During the 2017 Assembly about 600 speakers convened in more than 100 specialized sessions organized by individual countries, universities, research institutes, private companies and non-profit organizations.IMO scientists /about-imo/news/imo-at-the-arctic-circle-assembly-2017
  • 40. 2013_001_Nawri_et_al

    in a vertical plane, this is the component of the three-dimensional flow relevant for wind energy assessments. 13 The simulated data provide a good overview for the whole island. However, with a grid-point spacing of 3 km, the WRF model results are too coarse for a precise assessment of the wind con- ditions within a limited region, such as an individual valley or ridge, that may be appropriate /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

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