78 results were found for WA 0812 2782 5310 Bengkel Las Atap Canopy Baja Ringan Atap Go Green Kajoran Kab Magelang.

Results:

• 51. vanRoosmalen_etal-2009-WRR_2007WR006760

  and evapotranspiration to the surface and groundwater system. The vegetation type deter- mines the transpiration properties through the crop factor and the root depth, and the fraction of precipitation that is intercepted by the canopy. Land use changes can therefore reduce or amplify future climate change induced hydrological impacts in a catchment. [3] A number of studies have focused on the effects /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 52. Update on the earthquake swarm in Geldingadalir

  there were around 1300 earthquakes detected in the Reykjanes peninsula as a whole. This is a lot less than the day before when around 2300 earthquakes were detected. The scientific Advisory board for the civil protection services met on the 27th of December to go over the situation near Fagradalsfjall. GPS instruments and satellite interferograms show that the magmatic intrusion is limited /about-imo/news/update-on-the-eruption-in-geldingadalir

• 53. Update on the earthquake swarm in Geldingadalir

  there were around 1300 earthquakes detected in the Reykjanes peninsula as a whole. This is a lot less than the day before when around 2300 earthquakes were detected. The scientific Advisory board for the civil protection services met on the 27th of December to go over the situation near Fagradalsfjall. GPS instruments and satellite interferograms show that the magmatic intrusion is limited /about-imo/news/update-on-the-eruption-in-geldingadalir/

• 54. Factsheet_Bardarbunga_20141208

  continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash-producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier. If such an eruption would be prolonged it could eventually produce /media/jar/Factsheet_Bardarbunga_20141208.pdf

• 55. Factsheet_Bardarbunga_20141210

  scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier /media/jar/Factsheet_Bardarbunga_20141210.pdf

• 56. Factsheet_Bardarbunga_20141212

  scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier /media/jar/Factsheet_Bardarbunga_20141212.pdf

• 57. Factsheet_Bardarbunga_20141216

  of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier. If such an eruption would be prolonged it could eventually produce a lava flow.  Volcanic eruption /media/jar/Factsheet_Bardarbunga_20141216.pdf

• 58. Factsheet_Bardarbunga_20141219

  of the Bardarbunga caldera is still significant. Three scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive /media/jar/Factsheet_Bardarbunga_20141219.pdf

• 59. Factsheet_Bardarbunga_20141222

  and the rate of the subsidence of the Bardarbunga caldera is still significant. Three scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption /media/jar/Factsheet_Bardarbunga_20141222.pdf

• 60. Factsheet_Bardarbunga_20141230

  of the subsidence of the Bardarbunga caldera is still significant. Three scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive /media/jar/Factsheet_Bardarbunga_20141230.pdf