74 results were found for WA 0821 1305 0400 Biaya Buat Rumah Biaya 75 Juta Solear Kab Tangerang.

Results:

41. 2010_016

and autumn. The increase of annual glacier melt, assuming unchanged glacier geometry, is predicted to be in the range from 75–150% depending on scenario. This leads to a late summer discharge maximum caused by increased glacier runoff. The discharge peaks caused by snowmelt and glacier melt will become more distinct and appear as two separate summer maxima with the one caused by glacier melt /media/ces/2010_016.pdf
42. Paper-Olafur-Rognvaldsson_91

balance data from all the ice caps. REFERENCES Björnsson, H., Pálsson F., Guðmundsson M. T. and Haraldsson H. 1998. Mass balance of western and northern Vatnajökull, Iceland, 1991–1995, Jökull, 45, 35–58. Björnsson, H., Pálsson F. and Haraldsson H. 2002. Mass balance of Vatnajökull (1991–2001) and Langjökull (1996–2001), Iceland. Jökull, 51, 75–78. Bromwich, D. H., Bai L. and Bjarnason G. G. 2005 /media/ces/Paper-Olafur-Rognvaldsson_91.pdf
43. Hare-2011-ParticipatoryModelling

ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec ied .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
44. vanRoosmalen_etal-2009-WRR_2007WR006760

The hydraulic conduc- tivity of the sand formations is generally high, of the order of 104–103 m/s [Harrar et al., 2003; Sonnenborg et al., 2003]. In general, groundwater flows from east to west. At the water divide to the east the hydraulic head level is about 75 masl, decreasing to sea level at the west coast. The average head gradient is 0.001. The seasonal variation in head values is generally less /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
45. Bárðarbunga 2014 - December events

of the eruption column reached 3.1 km above Dyngjusandur, while the base of the aerosol-laden lower part of the plume reached ~1.4 km above the sand plain. Photo: Morten S. Riishuus. The lava extent is now just over 75 km², see map. For comparison, outlines based on a satellite image since 25.11. are given and the northern outline based on fieldwork 27.11. Institute of Earth Sciences. 1 /earthquakes-and-volcanism/articles/nr/3055
46. Bárðarbunga 2014 - December events

of the eruption column reached 3.1 km above Dyngjusandur, while the base of the aerosol-laden lower part of the plume reached ~1.4 km above the sand plain. Photo: Morten S. Riishuus. The lava extent is now just over 75 km², see map. For comparison, outlines based on a satellite image since 25.11. are given and the northern outline based on fieldwork 27.11. Institute of Earth Sciences. 1 /earthquakes-and-volcanism/articles/nr/3055/
47. Bardarbunga-2014_December-events

Board Notes from the meeting of the Scientific Advisory Board (pdf 0.4 Mb) On Dyngjusandur From Dyngjusandur, northeast of the vent, at 14:41 on 27 Nov 2014. The top of the eruption column reached 3.1 km above Dyngjusandur, while the base of the aerosol-laden lower part of the plume reached ~1.4 km above the sand plain. Photo: Morten S. Riishuus. The lava extent is now just over 75 km /media/jar/Bardarbunga-2014_December-events.pdf
48. BIAR_windrose_2005-2014

) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 62 7 29 6 22 9 11 0 4 5 3 0 1 6 2 3 2 9 3 6 5 1 4 6 5 7 8 9 12 9 19 1 22 8 25 9 34 9 30 2 18 0 6 4 5 4 4 0 4 4 3 2 2 5 2 7 1 8 4 5 12 6 26 1 35 1 54 1 75 0 81 3 Wind rose BIAR July 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 /media/vedur/BIAR_windrose_2005-2014.pdf
49. BIEG_windrose_2005-2014

110 100 2 4 6 8 10 Frequency of wind direction (%) Aerodrome Total observations: 7174 Calm: 12% Variable winds: 3.1% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 53 5 75 5 32 2 15 2 6 0 4 4 3 1 2 2 2 7 2 1 1 4 4 1 2 2 3 9 /media/vedur/BIEG_windrose_2005-2014.pdf
50. VI_2019_009

record is 60 km or 43% and 83% of them are over 20 km, out of range of the automatic station. 0% 10% 20% 30% 40% 0 10 20 30 40 50 60 70 Visibility [km] Propo rtion of record s 0% 25% 50% 75% 0 5 10 15 20 Visibility [km] Propo rtion of record s Figure 8. Records from the manual station. When every record over 20 km has been mapped to the range of the automatic station, 87% of the records show /media/vedurstofan-utgafa-2019/VI_2019_009.pdf