81 results were found for WA 0859 3970 0884 Pemborong Interior Rumah Luas Tanah 500 Meter Di Genuk Semarang.

Results:

11. Milly_etal-2008-Stationarity-dead-Science

data. The pdfs, in turn, are used to evaluate and manage risks to water supplies, water- works, and floodplains; annual global invest- ment in water infrastructure exceeds U.S.$500 billion (1). The stationarity assumption has long been compromised by human disturbances in river basins. Flood risk, water supply, and water quality are affected by water infra- structure, channel modifications /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
12. VED_AnnualReport-2013_screen

- meter stations, two fixed position weather radars and two mobile ones which are intended to monitor volcanic plumes. IMO operates over automatic snow depth sensors and conducts manned monitor- ing of snow-pack conditions, glacial margins and rivers; two stations are devoted to environmental monitoring. Many of these monitoring systems are operated in collaboration with other institutes /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
13. 2005EO260001

under Vatnajökull. However, neither the strain meter network nor other GPS stations detected the signal (Figure 1a). The upsurge in seismicity prompted IMO to warn the National Civil Protection Agency (NCPA) on 25 October that a jökulhlaup, and possibly a volcanic eruption, were imminent. This initi- ated NCPA’s lowest alert phase, the exploratory phase, which involves conferring /media/jar/myndsafn/2005EO260001.pdf
14. Factsheet-Bardarbunga-20140913

a meter over the last 24 hours.  The volcanic eruption in Holuhraun is still ongoing with similar strength as last few days. Lava flows at similar rates as yesterday towards East into Jökulsá á Fjöllum.  The lava filed was measured yesterday afternoon to be 24,5 square kilometres.  Accumulated volume of the lava is now estimated to be at least 200 million cubic meters.  Gas cloud from /media/jar/myndsafn/Factsheet-Bardarbunga-20140913.pdf
15. 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
16. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

(on CC impact s and )i s use d in publi c debate s (an di s no t distorted ) Raadgeve re t al .( 200 8) Ne w informatio n (on CC impacts )influence s polic y 24 .Decisio n suppor t syste m Rive rbasi n informatio n system s ar e u p to internationall y recognize d standard s (e.g .WB/UND P standards ) Youn g (200 2), Willi s an d Whittake r( 200 2) Climate change adaptation in European river basins /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
17. Press release on the l'Aquila sentence

30.10.2012 The International Association of Seismology and Physics of the Earth's Interior, IASPEI, has sent a press release on the l'Aquila sentence in Italy. The European Seismological Commission, ESC, has encouraged its representatives in numerous countries /earthquakes-and-volcanism/articles/nr/2568
18. VI_2016_006_rs

in a collaboration between the Austrian engineering company Ingenieurbüro Illmer Daniel e.U. (DI), Efla consulting engineers and the Icelandic Meteorological Office (IMO). Daniel Illmer carried out the analysis of landslide protection measures, Jón Kristinn Helgason, Tómas Jóhannesson and Eiríkur Gíslason wrote sections about the geographical setting, the land- slide history and the assessment /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
19. ces_geus_paakitsoq_full_report

+ 1 is calculated for every time-step and over each grid cell of the DTM according to Oerlemans (2001): bc(t+ 1) = bc(t) + braceleftBigg ∆t · (−Qm)/lm + Psolid if Qm > 0 Psolid if Qm ≤ 0 (1) where t is the discrete time variable, ∆t is the time-step, lm is the latent heat of fusion of ice (334 kJ kg−1) and Psolid is solid precipitation in meter water equivalent (m w.e.). The energy available /media/ces/ces_geus_paakitsoq_full_report.pdf
20. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

in the town of Horsens by 2,5 meter flooding. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 5 Figure 5 River basin Bygholm. Examples of challenges in the different sectors/areas Summery of challenges in sectors/subareas: Industrial Area Owners  Excess water from (heavy) rainfalls from roofs, roads and parking areas /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf