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

Results:

• 21. BIHN_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 68 0 62 9 111 2 167 0 117 5 70 6 26 7 25 4 58 7 47 3 36 6 101 3 91 1 53 1 117 0 73 6 44 2 72 7 38 7 60 4 113 6 70 0 109 3 130 5 26 1 12 5 30 0 14 4 10 5 34 6 17 0 29 4 114 3 158 0 146 5 172 7 Wind rose BIHN January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIHN_windrose_2005-2014.pdf

• 22. BIVO_windrose_2005-2014

  S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 26 8 27 9 44 9 36 0 111 1 173 2 39 3 24 9 20 7 9 0 2 9 4 7 1 0 1 4 3 3 1 6 2 6 3 5 6 8 10 1 27 3 39 0 86 7 209 6 71 4 25 7 21 5 8 2 5 4 9 4 2 9 7 7 11 8 7 1 16 0 21 5 Wind rose BIVO January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIVO_windrose_2005-2014.pdf

• 23. BIIS_windrose_2005-2014

  (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 28 6 85 3 223 1 339 5 367 0 315 2 161 9 89 4 34 6 11 7 18 7 9 7 7 7 15 9 8 7 7 2 14 9 7 4 22 6 36 9 69 6 148 3 183 1 148 5 96 9 45 1 21 1 9 3 7 8 2 0 1 7 2 4 1 2 1 6 7 3 11 6 Wind rose BIIS January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 /media/vedur/BIIS_windrose_2005-2014.pdf

• 24. Bardarbunga_kafli20140825

  : 115 km towards SW and 55 km towards NNE from Bárðarbunga Trend: Veidivötn fissure swarm NE-SW, Dyngjuháls fissure swarm NNE-SSW Ice cover: Partial Type of activity: Lava effusion, explosive phreatomagmatic Magma type: Basalt Eruption characteristics: Type of products: Airborne tephra, lava flows, water transported tephra VEI Max: VEI 5-6; most freq: VEI 1-2 Bulk volume /media/jar/Bardarbunga_kafli20140825.pdf

• 25. BIGR_windrose_2005-2014

  N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 41 6 40 6 37 9 30 4 36 6 43 5 36 4 56 2 72 3 56 9 54 0 38 8 25 9 27 3 19 3 15 6 17 0 11 0 9 8 8 9 11 9 11 3 15 0 26 1 28 4 28 0 16 6 13 4 24 6 22 9 15 5 17 0 17 2 17 1 28 3 38 9 Wind rose BIGR January 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 /media/vedur/BIGR_windrose_2005-2014.pdf

• 26. Perrels-CBA

  Authority 26.8.2011Adriaan Perrels/IL 22 CBA and MCA 26.8.2011Adriaan Perrels/IL 23 Structuring a CBA 1 Source: Eijgenraam et al 2001 Source: Commonwealth of Australia 2006 26.8.2011Adriaan Perrels/IL 24 Structuring a CBA 2 Project country Source: Eijgenraam et al 2001 Macro-economic full scale SCBA by effect type and source 26.8.2011Adriaan Perrels/IL 25 Applications • Assessing climate change /media/loftslag/Perrels-CBA.pdf

• 27. VI_2015_009

  J600v berg 2.utg) were also used in this study. Table 1. Main characteristics of river basins used in this study. River Name Type Area Mean Percentage Mean annual Period / (km2) elevation glacier precipitation for Gauging (m a.s.l) (mm) streamflow station (1961-2014) data vhm59 Ytri-Rangá L 622 365 0 1564 1961–2014 vhm64 Ölfusá L+D+J+S 5687 480 12.2 2003 1950–2014 vhm66 Hvítá (Borgarfirði) L+J 1577 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 28. AnneFleig_May2010_CES

  drought-supporting WTs over previous n days (n = 1, 15, 30, 45, 60, 90, 120, ... 330). Determination of the period of influence: dreg 90 45 little groundwater45 45 CES conference, Oslo, Norway, 31 May - 2 June 2010 210 60 45 60 highly productive aquifers moderately productive aquifers}90 210 60 60 Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe /media/ces/AnneFleig_May2010_CES.pdf

• 29. BITN_windrose_2005-2014

  12 22 12 36 43 2 1 21 42 10 5 18 5 21 29 10 19 15 10 4 7 Wind rose BITN February 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 1 2 3 4 5 Frequency of wind direction (%) Aerodrome Total observations: 740 Calm: 5.8% Variable winds: 7.6% Average wind speed for wind direction Wind direction (°) Wind /media/vedur/BITN_windrose_2005-2014.pdf

• 30. 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