87 results were found for x 북창동건마ŧ‘dm080.com” 북창동아로마 북창동오피♙북창동안마 북창동업소.

Results:

• 81. 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

• 82. 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

• 83. 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

• 84. 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

• 85. 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

• 86. Bardarbunga-2014_October-events

  earthquakes were observed in the dike intrusion and about 20 close to Herðubreið. The eruption can not be seen on the webcams. 9 October 2014 - a high definition image of the lava 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 /media/jar/Bardarbunga-2014_October-events.pdf

• 87. 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/