79 results were found for JZMOR contro la truffa: strategie efficaci per proteggere i tuoi fondi.

Results:

• 21. Case_B___Road_transport_operation_and_infrastructure_planning

  vuosille 2010–2040; Trafi 3/2010 Shares of elderly drivers without accidents and/or fines (in the previous year) by age category, and comparison with very young drivers Source: Mikkonen, V. (2010), Seniorikuljettajien seurantaindeksi, Trafi 5/2010 Aggregate risk of motor vehicle collision (per million vehicle km) in Finland (“dry” road vs. icy/snowy road surface) (2003-2006). (a) Based /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 22. 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

• 23. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  in climate change adaptation should reflect the nature of the uncertainty sources and how they interact with risk level and decision making: (i) epistemic uncertainties can be reduced by gaining more knowledge; (ii) uncertainties related to ambiguity can be reduced by dialogue Mitig Adapt Strateg Glob Change DOI 10.1007/s11027-012-9366-6 J. C. Refsgaard (*) Geological Survey of Denmark /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 24. 2010_003rs

  .............................. 49 Figure 3.19. The zigzag like structure of fault H2-05 in the Hengill area. ......................... 50 Figure 3.20. Fault H-02 in the Hengill area ....................................................................... 50 Figure 3.21. Seismicity and mapped faults in boxes G and I, Ölfus and Flói districts. ...... 52 Figure 3.22. Rake angle distribution for fault segments G-15, G-16 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 25. Kurpniece_Liga_CES_2010

  hydropower plants in Latvia produce approximately 50% of electricity consumed per year in the country. Climate change impacts on hydrological regime might have a significant effect on a hydropower production • To study the climate change impact on hydrological regime in Latvia river basins for the period 2021-2050 Methods and study area The Plavinas HPP on Daugava River and the Aiviekstes HPP /media/ces/Kurpniece_Liga_CES_2010.pdf

• 26. Adalgeirsdottir-etal-tc-5-961-2011

  of the glaciers. An up to 8 m thick winter snow layer was measured in the accumulation area (∼4 m w.e.). Ice melt of up 10 m w.e. was measured in the lowest part of the ab- lation zone in summer, and 2 m w.e. was melted during win- ter. Taking into account ∼2 m of annual rainfall, the runoff from this part of the glacier was estimated as ∼14 m w.e. per year; a surprisingly high value (Ahlmann, 1939 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 27. 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

• 28. VI_2020_004

  ....................................................................................... 99 APPENDIX I. Daily tephra dispersal simulation .................................................................... 102 APPENDIX II. HEKLA 1980 – The likelihood of receiving tephra at different locations .... 104 APPENDIX III. KATLA 1918 – The likelihood of receiving tephra at different locations ... 107 APPENDIX IV. ÖRÆFAJÖKULL 1362 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 29. 2010_005_

  period, and linear trends in degrees per decade within the 2004–50 period, for the IPCC GCM ensemble mean, the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. 23 2 Mean annual surface air temperature and total precipitation during the 1961–90 control period. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 24 3 Dependence on terrain elevation of surface air temperature /media/ces/2010_005_.pdf

• 30. Keskitalo_et_al-MLG_and_adaptation_FINAL

  /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf