60 results were found for WA 0821 1305 0400 Kontraktor Pasang Interior Rumah Type 60 2 Lantai Di Cibodas Kota Tangerang.

Results:

• 31. VI_2014_001

  6 0 20 40 60 80 10 0 12 0 14 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm51 heM 95?bh ??Obs 95?bh ??W aSiM 95?bh heM Annual max. Q : GEV Distributions for vhm51 Index flood model no. 6 l l l l l l l l l l l l l l l l l l −2 0 2 4 6 0 50 10 0 15 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm52 heM 95?bh Obs 95?bh /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 32. VI_2020_004

  is presented in Table 2. The table shows which type of data would be available during the different phases of a volcano reactivation timeline. Which type of products would be produced according to the data and the usage of these products is also reported as function of time. In this representation a long-term hazard assessment evolves into a short-term hazard assess- ment and possibly even further /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 33. 2010_016

  -based and 10 based on IPCC GCM simulations. The choice of the GCM models was based on their SAT performance for the present-day climate near Iceland as mentioned above. 2. For GCM-based scenarios, temperature change in the highland interior of Iceland, where the large ice caps are located, were increased by 25% based on the results of RCM downscaling (Nawri & Björnsson, 2010). 3. Expected /media/ces/2010_016.pdf

• 34. VI_2019_009

  .............................................................................................. 45 5.3 Present weather ..................................................................................... 45 Appendix ......................................................................................................... 47 5 List of Figures 1 How PWD22 determines the type of precipitation. ........................................ 11 2 Number of records as a function of the height /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 35. IMO_AnnualReport2014

  The map shows the likelihood at a specific location, that the hourly ground concentration of SO2 will exceed a threshold of 2600 µg/m3 dur- ing summer season. The colour scale shows di?rent values (likelihood smaller than 1% has no colour associated). I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 7 In the evening of 21 July 2014 a large rockslide oc- curred in Askja /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 36. Journal_of_Hydrology_Veijalainen_etal

  countries in hydrological climate change studies, and in Scandinavia HBV is the most commonly used model type (Vehviläinen and Huttunen, Table 2 Climate scenarios used in the study (Finnish Meteorological Institute, ENSEMBLES data archive) and their projected annual changes in temperature and precipitation in Finland by 2070–2099 compared with the reference period 1971–2000. The greatest /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 37. norsem_janutyte

  Fault plane solutions of the earthquakes in Nordland, Norway Ilma Janutyte(1), Jan Michalek(2), Conrad Lindholm(1), and Lars Ottemoller(2) (1) NORSAR, Kjeller, Norway, (2) University of Bergen, Bergen, Norway This study is a part of the ongoing NEONOR2 project which is carried out in Nordland, norther Norway. This work aims to define the fault plane solutions (FPS) of the earthquakes /media/norsem/norsem_janutyte.pdf

• 38. Factsheet_Bardarbunga_140914

  breaking out from the main lava stream towards the east and west. The largest one of these lava tongues stretches towards the east and had become 300 m wide and 2 km long at 18:00 yesterday. An eruption cloud reaches 4 km in height but lowers with distance from the eruption site.  Seismic activity is similar to what it has been in the past days but earthquakes are starting to go down in numbers /media/jar/myndsafn/Factsheet_Bardarbunga_140914.pdf

• 39. BIBD_windrose_2005-2014

  Wind rose BIBD 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 Frequency of wind direction (%) Aerodrome Total observations: 18358 Calm: 9.5% Variable winds: 1.7% 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 /media/vedur/BIBD_windrose_2005-2014.pdf

• 40. Forecasts - Nautabú

  Cloud cover: 70% 20 GMT 0° NNW 5 Cloud cover: 100% 21 GMT -0° NNW 4 Cloud cover: 100% 22 GMT -1° NNW 3 Cloud cover: 100% 23 GMT -1° NW 2 Cloud cover: 100% Tue 2.05 00 GMT -1° NW 2 Cloud cover: 100% 01 GMT -1° NW 2 Cloud cover: 60% 02 GMT -2° WNW 2 Cloud cover: 60% 03 GMT -1° WNW 2 Cloud cover: 90% 04 GMT -1° WNW 2 Cloud /m/forecasts/areas