79 results were found for WA 0821 1305 0400 RAB Pembangunan Rumah Type 36/60 1 Lantai Jakarta Pusat.

Results:

• 61. Glacial outburst floods

  also Catalogue of Icelandic volcanoes. Jökulhlaups can be of various sizes, where the maximum discharge and volume of floodwater spans orders of magnitudes. The largest jökulhlaups in historic times, (e.g. outbursts from Mýrdalsjökull caused by Katla eruptions), have had a maximum discharge on the order of 100.000 m3s-1, comparable to the discharge of the Amazon river. The rate of discharge /volcanoes/volcanic-hazards/glacial-outburst/

• 62. VI_2014_006

  0 0 20 12 % Grassland <1 43 25 10 25 % Woodland <1 0 0 2 2 % Moss 59 25 0 14 13 % Little or no vegetation 35 27 30 63 36 % Wetland 0 5 46 6 7 % Lakes 6 <1 <1 <1 3 300 400 500 600 700 800 30 0 40 0 50 0 60 0 70 0 km km 2400 2200 2000 1800 1600 1400 1200 1000 800 600 400 200 0 m.a.s.l Watershed Glacier vhm19 vhm10 vhm26 vhm64 vhm66 Figure 1. Topography of Iceland and location of the watersheds /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 63. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  process in which the effect of adopted water management measures must be monitored and adjusted in an iterative way as new information and technology gradually become available under changing and uncertain external impacts, such as climate change. This paper identifies and characterises uncertainty as it occurs in the different stages of the IWRM process with respect to sources, nature and type /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 64. vanRoosmalen_etal-2009-WRR_2007WR006760

  of the land use types are provided in Table 2. The parameters for grain vary throughout the 136 days of the growing season, which starts on 1 April and ends 15 August each year. The growing season is divided into four stages, with maximum values of the leaf area index (LAI) and root depth (dr) from day 60 until harvest. From day 60 the crop factor Kc for grain equals 1.05 and then increases /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 65. Observations - Akureyri

  GMT 1.4° N 6 Max wind : 8 / 14Sunny (3/8)Visibility 60 kmPrecip.: 0.0 mm / 1 h 17 GMT 1.5° N 12 Max wind : 12 / 16Precip.: 0.0 mm / 1 h 16 GMT 1.8° N 11 Max wind : 11 / 15Precip.: 0.0 mm / 1 h 15 GMT 3.5° N 5 Max wind : 6 / 10Sunny (2/8)Visibility 60 kmPrecip.: 0.0 mm / 1 h 14 GMT 2.6° N 8 Max wind : 8 / 10Precip.: 0.0 mm / 1 h 13 GMT 3.6 /m/observations/areas

• 66. Kriauciuniene_Jurate_CES_2010

  0 1 9 8 0 2 0 0 0 -40 -25 -10 5 20 35 50 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 -30 -15 0 15 30 45 60 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 -35 -20 -5 10 25 40 55 70 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 -40 -25 -10 5 20 35 50 65 80 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 -40 -25 -10 5 20 35 50 65 80 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 -55 -40 -25 -10 5 20 35 50 1 9 2 0 1 9 4 0 1 9 6 0 1 /media/ces/Kriauciuniene_Jurate_CES_2010.pdf

• 67. Windspeed

  Baldur Ragnarsson 29.4.2008 Windspeed conversions The Icelandic Meteorological Office uses the SI (Systeme Internationale d´Unites) unit metres per second (m/s) in windspeed measurements. Here you can convert between different units of windspeed. Type a number into a textbox below and then click outside it. Please note that Beaufort-values are between 0 and 12. Beaufort /weather/articles/nr/1283

• 68. Windspeed

  Baldur Ragnarsson 29.4.2008 Windspeed conversions The Icelandic Meteorological Office uses the SI (Systeme Internationale d´Unites) unit metres per second (m/s) in windspeed measurements. Here you can convert between different units of windspeed. Type a number into a textbox below and then click outside it. Please note that Beaufort-values are between 0 and 12. Beaufort /weather/articles/nr/1283/

• 69. norsem_korja

  Observations on Intraplate Seismicity in Central Fennoscandia Korja, A.1, Uski, M.1, Lund, B.2, Grigull, S.3, Nironen, M.4, E., Högdahl, K.2 1University of Helsinki, Institute of Seismology, Helsinki, Finland, annakaisa.korja@helsinki.fi 2University of Uppsala, Uppsala, Sweden 3Geological Survey of Sweden, Uppsala, Sweden 4Geological Survey of Finland, Espoo, Finland Fennoscandian Shield /media/norsem/norsem_korja.pdf

• 70. 2010_012rs

  center. The pass-band is within 0.075 to 3 Hz and is applied to both velocity and acceleration records, whereas in ElarmS the acceleration record is only low-pass filtered (Allen and Kanamori, 2003; Shieh et al., 2008). The process was implemented on 9 stations of the SIL seismic network at month 36 (see Figure 1). The SIL network consists mostly of combinations of short-period sensors /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf