59 results were found for WA 0821 1305 0400 Spesialis Rumah Minimalis 2 Lantai Type 36/60 Berpengalaman Tapos Kota Depok.

Results:

• 41. 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

• 42. BIRK_windrose_2005-2014

  Total observations: 7284 Calm: 1.1% Variable winds: 1.3% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 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 12 3 36 9 29 2 14 2 13 8 13 2 17 7 46 2 70 8 60 8 41 6 28 9 27 5 23 1 26 4 20 1 18 4 17 3 13 8 12 4 15 6 15 4 11 9 8 6 12 6 10 0 11 /media/vedur/BIRK_windrose_2005-2014.pdf

• 43. VI_2020_004

  ................................................................................. 60 Figure 34 Probabilistic hazard map for a tephra load ≥0.1 kg/m2 (Katla) ............................... 62 Figure 35 Probabilistic hazard map for a tephra load ≥1 kg/m2 (Katla) .................................. 63 Figure 36 Probabilistic hazard maps for a tephra load ≥10 kg/m2 (Katla) .............................. 64 Figure 37 Probabilistic hazard maps for a tephra load ≥100 kg /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 44. VI_2013_008

  combinations indicate the type of river, with the first letter indicating the primary type. Direct runoff river (D), presence of lakes (S), glacier-fed river (J), groundwater (L). Gauging station vhm vhm vhm vhm vhm vhm 19 10 26 145 66 64 Name Dynjandisá Svartá Sandá Vestari- Hvítá Ölfusá Jökulsá Type of river D+L D+L D+L D+J+L L+J L+D+J+S Drainage area (km 2) 42 397 267 850 1664 5687 Mean altitude (m a.s.l /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 45. Group5-Participation_stages

  1 Stakeholders involvement – Participation stages Participation stage Duration stakeholders Participatory level Type of knowledge Knowledge elicitation 1 Problem identification (Stakeholder analysis) 2 months  Horsten municipality (Competent authority) n.a 2 Information provision 2 months  Horsten municipality  Policy maker  Insurers  Neighbouring municipality /media/loftslag/Group5-Participation_stages.pdf

• 46. 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

• 47. VI_2009_012

  Appendix – near-field constraint ........................................................................................ 35  III Appendix – PGV and PGA versus distance for all events ................................................. 36  List of figures Figure 1. Map of SW Iceland showing the epicenters of 46 earthquakes used in the study.. 10  Figure 2. CMT-moment magnitude estimates vs /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 48. CES_D2.4_task1

  change signal, with higher (lower) probabilities in the north (south). At this time, typically about 60% of all months are projected to be wet in northern Europe, although with a substantial variation with the time of the year (generally least wet 2 In this case, observations were only used up to the year 2002 because of the reason discussed /media/ces/CES_D2.4_task1.pdf

• 49. Observations - Skjaldþingsstaðir

  Observations - Skjaldþingsstaðir | Observations | Icelandic Meteorological office Observations - Skjaldþingsstaðir Mon 1.05 14 GMT 2.1° E 1 Max wind : 1 / 2 13 GMT 1.9° NE 1 Max wind : 2 / 2 12 GMT 0.8° SSW 2 Max wind : 3 / 5OvercastVisibility 20 km 11 GMT 0.8° S 1 Max wind : 3 / 4 10 /m/observations/areas

• 50. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  behavior towards a public good based on individual preferences, and provides insights into the type of indi- viduals who best serve the social interest and those to avoid in institutional settings. This distinction helps us to understand why, with the same incentives, the provision of public goods works better in some populations than in others. In addition, our use of a sequential public good /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf