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

Results:

• 41. The weather in Iceland 2007

  warmest recorded, but in the Northeast and East it was among the 15 warmest. Multi-station temperature measurements go back to the early 1870s. In Reykjavik only May had slightly below normal temperatures (1961-1990) and in 7 of the months the temperature was more than 1.5°C above the normal. April and July were particularly warm and April registered the highest temperature ever measured in April /about-imo/news/2008/nr/1205

• 42. The weather in Iceland 2007

  warmest recorded, but in the Northeast and East it was among the 15 warmest. Multi-station temperature measurements go back to the early 1870s. In Reykjavik only May had slightly below normal temperatures (1961-1990) and in 7 of the months the temperature was more than 1.5°C above the normal. April and July were particularly warm and April registered the highest temperature ever measured in April /about-imo/news/nr/1205

• 43. Milly_etal-2008-Stationarity-dead-Science

  6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 44. “The small eruption” in

  to measure the composition and the flux rate”, says Melissa.Figure 8. Gas is one of the hazards from the volcano. The specialists from IMO go regularly to the eruption site to measure the composition and emission rate of the gases. They need to wear special equipment to protect themselves from the gas and to make the measurements. In the photo Melissa Anne Pfeffer is preparing Baldur Bergsson /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months

• 45. “The small eruption” in

  to measure the composition and the flux rate”, says Melissa.Figure 8. Gas is one of the hazards from the volcano. The specialists from IMO go regularly to the eruption site to measure the composition and emission rate of the gases. They need to wear special equipment to protect themselves from the gas and to make the measurements. In the photo Melissa Anne Pfeffer is preparing Baldur Bergsson /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

• 46. Lava flows

  : Type of the magma and its viscosityThe steepness of the slope surface.If the magma flows as one big spread or in a narrow channel or a magma tunnel.The rate of the magma coming from the ventBasaltic magma can flow tens of kilometers from the eruption vent and the margin of the lava can go up to 10 km/hour depending on slope. Usually the transport time is shorter, but if the slope gradient /volcanoes/volcanic-hazards/lava-flow/

• 47. ESC-IASPEI-statement-LAquila-2012-1

  of IASPEI's most brilliant scientists, who dedicated their lives to the reduction of seismic risk and to whom go our sympathy and support. , on behalf of the world community of seismologists, expresses its deepest concern for the L’Aquila verdict and prison sentence, that condemns for involuntary manslaughter seven prominent Italian scientists and members of the Great Risks Commission /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 48. Moberg_Anders_CES_2010

  1500 years and IPCC future temperature scenarios • Significant climate changes have occurred in the last millennium – affecting both temperature and hydrology • Future changes in this century will likely go substantially beyond what we have seen in the recent past IPCC 2007, SPM Fig. 5Mann et al. Science 2009, 326, p.1257, Fig. 1 /media/ces/Moberg_Anders_CES_2010.pdf

• 49. norsem_slunga

  are as large as the friction allows) directly leads to boundaries on the k-values and that these curves not only has a simple physical meaning, they also show a significant difference from the numerical fitting. This encouraged me to later go on and use the same assumptions to put boundaries on the pore pressure within wet crust which then was the base for the QuakeLook complete stress /media/norsem/norsem_slunga.pdf

• 50. Hare_2-participation

  and groups come and go frrom processes (how do you keep them turning up year after year?) • Participatory burn-out – legislators want it everywhere – too often with not enough results 5. Overselling of participation the tyranny of participation? Cooke & Kothari (2000) • Experiences in Cooperation and Development projects – Ignorance of existing power structures in local communities • Which /media/loftslag/Hare_2-participation.pdf