78 results were found for WA 0821 1305 0400 Total Biaya Pemasangan Moulding Dinding Kamar Di Kota Depok.

Results:

• 11. Paper-Olafur-Rognvaldsson_92

  ) and Jónsdóttir (2008). Therefore, comparison of measured and simulated water balance cannot be di- rectly used for validation of the model-generated precipitation. According to the non-scaled MM5 output for the period 1961–1990, mean precipitation for the whole of Iceland was 1790 mm y−1. After scaling the precipitation, this value was reduced to 1750mm y−1, i.e. by approximately 2%. This difference /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 12. 2010_017

  an important part of the runoff from many areas. In total, approximately 20% of runoff in Iceland originates from groundwater (Hjartarson, 1994a). In the above mentioned previous simulation of runoff map for Iceland for the period 1961– 1990, groundwater was omitted. Effects of groundwater flowing across watershed boundaries were simulated by scaling the precipitation for each watershed. On watersheds /media/ces/2010_017.pdf

• 13. VI_2009_006_tt

  the maximum discharge of jökulhlaup water at the glacier terminus is estimated as 97 m3 s 1. This jökulhlaup was a fast-rising jökulhlaup as other jökulhlaups in Skaftá and cannot be described by the traditional Nye-theory of jökulhlaups. The total volume of flood water was estimated as 53 Gl. The average propagation speed of the subglacial jökulhlaup flood front was found to be in the range 0.2–0.4 m s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 14. VI_2014_005

  incorporated into the CORINE Land Cover 2006 (CLC2006) inventory (Árnason and Matthíasson, 2009). In the model, the total land area (95,570 km2) is broken down into the following surface types (percentages of terrain type coverage refer to the total model land area): Sparse tundra: 39,421 km2 (41.3%) Tundra: 23,688 km2 (24.8%) Subpolar pastures: 11,364 km2 (11.9%) Permanent snow: 10,046 km2 (10.5 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 15. Avalanche notices last 10 days

  Number Faxaflói1Breiðafjörður0West fjords0North West0North East0Eastern coastal area0East fjords0South East 0South0Central highlands0 Total:1 Last 24 hours Region Number /avalanches/notifications/

• 16. VI_2021_008

  methodology is widely utilized by many automatic earthquake detectors, but instead of having window lengths on the order of minutes, like the ALERT module, they have window durations on the order of seconds. A longer STA window duration will make the module less sensitive to small signals (Trnkoczy, 1999). Additionally, the total duration of the STA and LTA windows may not exceed 24 hours /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 17. Total cloud cover

  Total cloud cover Total cloud cover Lower clouds Middle clouds High clouds Composite /weather/aviation/cloudcover/ecmwf-model/

• 18. Journal_of_Hydrology_Veijalainen_etal

  into three categories: those characterized by numerous lakes in the central part of the country; small and medium sized coastal rivers; and large and medium sized rivers of northern Finland (Fig. 1b) (Mustonen, 1986; Korhonen and Kuusisto, 2010). Thousands of lakes (4500 over 0.5 km2 and 188,000 lakes of at least 0.05 ha) that cover about 10% of the total area of Finland give the watersheds in central /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 19. 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

• 20. Refsgaard_etal-2007-Uncertainty-EMS

  from computer implementation of the model, e.g. due to numer- ical approximations, resolution in space and time, and bugs in the software. The total uncertainty on the model simulations, model output uncertainty, can be assessed by uncertainty propagation taken all the above sources into account. 3.3. Nature of uncertainty Walker et al. (2003) explain that the nature of uncertainty can /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf