89 results were found for X 정보이용료현금화 ≰ㅋr톡 1SEC≱ 티켓타카 Y 정보이용료현금화 전문 포탈 지난해🛤manoeuver/.

Results:

• 51. 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

• 52. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 53. VI_2013_008

  when local information alone (method 2) is not sufficient. In order to take into account seasonal effects, a moving window of +/– 45 days centered on the target day was considered for the selection of analogues, so that in an archive made of Y years, each target day was at most associated to Y x 91 potential analogues. The window size was arbitrarily defined and not optimized. A similar window /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 54. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 55. VI_2009_013

  is based on Moho reflections from the location marked by the X (Vogfjörd et al., 2002). 11 Figure 2. Upper: Cumulative number of earthquakes in and near to Eyjafjallajökull. Lower: Magnitude distribution (local moment magnitude scale, Mlw). 1.2 Seismic activity and deformation of the volcano The number of detected earthquakes in Eyjafjallajökull has risen substantially since /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 56. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  from the glacier margins). This was done by shifting the x and y coordinates of the 40 m40 m DEMs in 5 m steps and calculating the correlation to the corresponding values of the 5 m5 m EMISAR DEM. In all cases, both the maximum correla- tion and minimum standard deviation yielded the same shift. After the co-registration, the same ice-free areas were used to correct the vertical offset of the DMA /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 57. TietavainenHanna_CES_2010

  and objective CES Conference, Oslo 31.5.-2.6.2010 Study area • Two study areas sized 100 x 100 km located in north-eastern (NE) and south-western (SW) part of Finland • Climatologically different zones: • NE: • between middle- and north-boreal zones • continental climate • SW: • between hemi- and south-boreal zones • maritime influence • Past and future monthly precipitation sums in May-September /media/ces/TietavainenHanna_CES_2010.pdf

• 58. Case_B___Road_transport_operation_and_infrastructure_planning

  variability Models Emission scenarios 2000 2100 LEVEL OF UNCERTAINTY Near future End of the century Natural climate variability + + Climate model sensitivity (+) ++ Emission scenarios ++ Source: J. Räisänen (Univ. of Helsinki) Probabilistic forecasts of temperature change in southern Finland (1971-2000 barb2right 2011-2020) Temperature change (ºC) P r o b a b i l i t y d e n s i t y ( 1 / º C /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 59. Ash measurements

  in estimating the height of the plume. At this time, the plume reached heights of 8 - 12 km. During the 2010 Eyjafjallajökull eruption, the weather radar proved to be a very useful tool, but the great distance to the eruption site (160 km) reduced the quality of the data. Therefore, a mobile X-band weather radar was purchased, but while this custom made radar was being assembled and tested, another /about-imo/news/nr/2183

• 60. Articles

  and might thus still change. Further, the y-scale is logarithmic, which means that one step on the scale accords to a factor of 10. Of interest - Bárðarbunga Reduction of the accesscontrolled area around Holuhraun lava field END OF ERUPTION declaredby the Scientific Board Location map /earthquakes-and-volcanism/articles/bigimg/3039