70 results were found for WA 0852 2611 9277 Biaya Bikin Interior Meja Dapur Set Apartemen Gandaria Heights Jakarta Selatan.

Results:

• 41. Final estimates of the emissions from the Holuhraun eruption based on ground-based measurements

  of the heat released by the Holuhraun lava field. This dust encouraged the formation of clouds that persisted over the eruption site as other clouds moved past. In general, the start of the eruption was the strongest with the highest eruption cloud heights, and then for the duration of the eruption, until the end, the height varied mainly between 1–3 km agl. The eruption cloud height has a major /about-imo/news/final-estimates-of-the-emissions-from-the-holuhraun-eruption-based-on-ground-based-measurements-now-published

• 42. Eyjafj_status_2010-04-27

  crater is ~50 m lower than the surrounding ice cauldron. Volcanic spatter was observed from the vent, with ejected lava reaching heights of 100–200 m. Unstable plumes of ash rise regularly from the vent. Lava continues to flow to the north, advancing ~1 km from the crater. Depressions in the ice-surface have formed due to lava being in contact with ice; these features have enlarged considerably /media/jar/myndsafn/Eyjafj_status_2010-04-27.pdf

• 43. Grimsvotn_status_2011-05-30_IES_IMO

  Since Thursday the tremor had been intermittent. Today, Monday 30 May, it has been confirmed by the participants of Iceland Glaciological Society's spring expedition that the eruption has ended. The end of the Grímsvötn eruption is set to 7 UTC Saturday morning 28 May 2011. /media/jar/Grimsvotn_status_2011-05-30_IES_IMO.pdf

• 44. Adalgeirsdottir-etal-tc-5-961-2011

  the set- tlement, glaciers were smaller than at present. They started to advance in the 13th century at the onset of the Little Ice Age that lasted until late 19th century when most glaciers in Iceland reached their maximum extent. In the 20th century, the climate was significantly warmer than during the Little Ice Age, with higher temperatures in the period 1930–1945 and again at the end /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 45. vonKorff_etal-2010

  ). a71 There are other stakeholders who may need to be involved in the design and then in the participation process itself. a71 There is a set of contextual factors that need to be taken into consideration when designing the participation plan. These can include existing levels of conflict among stakeholders, their previous experiences with participation, relevant legal or regulatory settings /media/loftslag/vonKorff_etal-2010.pdf

• 46. Hare-2011-ParticipatoryModelling

  - work. The second half of the article discusses the potential for participatory modelling to progress from being a mainly research-driven activity in the water sector to one being adopted for widespread use by water managers. By widespread adoption I mean that participatory modelling becomes mainstream in the sector and that managers set up their own organizing teams, independent of researchers /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 47. BIIS_windrose_2005-2014

  1 6 Wind rose BIIS March 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 12 Frequency of wind direction (%) Aerodrome Total observations: 2611 Calm: 9.8% Variable winds: 16% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N /media/vedur/BIIS_windrose_2005-2014.pdf

• 48. GA_2009_91A_4_Andreassen

  - elled using precipitation data southwest of the gla- cier. Results from the model compared well with re- ported mass balance values for the period 1949– 2006, obtained correlations (r) for bw and bs varied between 0.83 and 0.87 depending on model set up. Reconstruction of the mass balance series for the period 1924/1925–1948/1949 suggested a cumula- tive mass deficit of c. 30 m w.e. mainly due /media/ces/GA_2009_91A_4_Andreassen.pdf

• 49. VI_2020_004

  volcanological scenario (typified by mass of erupted magma, the plume height, the dimension of tephra, duration of the event) was chosen and simulated by using a large data set of meteorological conditions. For Hekla the scenario is the1980 eruption, for Katla it is the 1918 eruption and for Öræfajökull it is the 1362 eruption. Input parameters for the dispersal model have been defined in order /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 50. 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