86 results were found for x 의정부핸플ゥ《anmaya135.com》♨남양주안마 광명안마 오피한국♙오피어때♣오산휴게텔.

Results:

• 71. Eriksson_Garvill_Nordlund_2006

  asked questions about perceived fairness, effectiveness, expected reduction ARTICLE IN PRESS e (1 is a ’ e m n orde , raised tax on fuel (TAX), and improved public transport (PUB)). X/PUB to be a fair measure?’ t driving distance, do you think other car drivers in your municipality e is implemented?’ t driving distance, do you think you would reduce car use if the measure is X/PUB to affect your /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 72. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 73. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 74. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 75. 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

• 76. VI_2020_008

  Útreikningarnir eru í 2,5 x 2,5 km neti á 1 klukkustundar fresti fyrir tímabilið september 1979 til desember 2016. Einnig eru notaðar sjálfvirkar úrkomumælingar frá 49 stöðvum sem allar hafa mælt samfellt í yfir 10 ár. Í báðum tilvikum er um daggildi að ræða, þ.e. uppsafnaða úrkomu frá miðnætti til miðnættis. Í næmniathugunum eru mælingar frá 12 stöðvum, svokölluðum kjarnastöðvum, skoðaðar /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 77. Update on activity in Eyjafjallajökull 2010

  plumes are seen somewhat lower and mark the front of the lava stream. The size of the eruptive crater is 280 x 190 m. Lava splashes are thrown at least a few hundred meters into the air. Overall assessment is that it is more explosive activity and ash production than was observed yesterday. Progression of the lava seems to be slower than yesterday. Presently there are no indications /earthquakes-and-volcanism/articles/nr/1884

• 78. Bárðarbunga 2014 - October events

  Holuhraun lava field Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather and visibility, shows the outlines of the new lava in exceptionally high detail (see full image) as they were two days ago. Referral: (c) DLR/ Fjarkönnun ehf./IsViews 10/2014. 9 October /earthquakes-and-volcanism/articles/nr/3011

• 79. 2010_016

  the following five parameters were adjusted: (1) Storage coefficient of direct runoff kd; (2) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X /media/ces/2010_016.pdf

• 80. 2010_017

  ) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X and Y direction. The hydraulic conductivity is adjusted in distributed grids unlike /media/ces/2010_017.pdf