29 results were found for WA 0821 1305 0400 Ongkos Jasa Jendela Aluminium Sliding Kelapa Gading Jakarta Utara.

Results:

• 11. Hofsjökull ice cap gains mass

  the past 2 decades. Summer ablation was found to be less than 50% of the 1995 - 2014 average. Fig. 3 (enlarge). Ablation stake (white) near the northern margin of Hofsjökull on October 9th 2015 at a height of 980 m. A yellow indicator gives the height of the aluminium stake, whereas the red bar shows the typical stake height during years with negative mass balance. Photo: Bergur Einarsson /about-imo/news/nr/3229

• 12. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf

• 13. askja_minnisblad_ens

  means that the failure surface of the slide is concave. The volume of the slide is roughly estimated 30–50 million m3, however, the estimation may change when further measurements and analyses have been carried out, especially on the part that is in the lake and regarding the depth of the sliding surface. If the bottom of the slide reaches below the lake bottom, the total volume of material /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 14. 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

• 15. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  of the slide is concave. The volume of the slide is roughly estimated 30–50 million m³, however, the estimation may change when further measurements and analyses have been carried out, especially on the part that is in the lake and regarding the depth of the sliding surface. If the bottom of the slide reaches below the lake bottom, the total volume of material that moved may be a lot more /avalanches/articles/nr/2929

• 16. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  their audience. Climatic Change (2012) 112:233–242 DOI 10.1007/s10584-011-0205-7 C. S. Weiler (*) Office for Earth System Studies, Whitman College, Walla Walla, WA 99362, USA e-mail: weiler@whitman.edu J. K. Keller School of Earth and Environmental Sciences, Chapman University, Orange, CA 92866, USA C. Olex The Point, 121 Jewett Street, Newton, MA 02458, USA 1 Introduction Of all the applications /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 17. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 18. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 19. Kok_JGEC658_2009

  /media/loftslag/Kok_JGEC658_2009.pdf

• 20. IMO_AnnualReport2014

  measurements and analyses have been carried out, especially on the part that is in the lake and regarding the depth of the sliding surface. If the bot- tom of the slide reaches below the lake bottom, the total volume of material that moved may be a lot more. The water level of Lake Öskjuvatn rose 1–2 m after the rockslide. The rise of the water level will be measured precisely because it gives /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf