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

Results:

• 41. 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

• 42. VI_2013_008

  Probabilistic daily streamflow forecast using an analogue sorting method Philippe Crochet VÍ 2013-008 Report Probabilistic daily streamflow forecast using an analogue sorting method VÍ 2013- 008 ISSN 1670- 8261 Report? +354 522 60 00 vedur @vedur . is Veður st of a Íslands Búst aðaveg ur 7 – 9 150 Reyk j avík Philippe Crochet, Icelandic Met Office   Contents 1 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 43. 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

• 44. 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

• 45. CES_D2.4_task1

  264 OKSOEY FYR NO +58:04:00 +08:03:02 9 TP 265 BERGEN FLORIDA NO +60:22:59 +05:19:59 12 TP 266 BODOE VI NO +67:16:01 +14:21:32 11 TP 302 TRANEBJERG OST DK +55:51:00 +10:36:00 11 P 303 VESTERVIG-1 DK +56:46:00 +08:19:00 18 T 304 NORDBY (FANO)-1 DK +55:27:00 +08 /media/ces/CES_D2.4_task1.pdf

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

  +2αi )1+αi ) 1−ri + (1 − pi1)(10 + 0.6xi1)1−ri 1 − ri (11) The first mover’s beliefs about the second mover’s type, i.e., the second mover’s β , and her risk aversion both affect the optimal contribution. Depending on the second mover’s choice, the first mover may earn the same as or less than the second mover. Regarding inequity preferences, only the first mover’s disadvantageous inequity aversion /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 47. Wind, temperature and precipitation forecasts

  ;script type="text/javascript" src="http://vedur.is/js/iframe.js"></script> <script type="text/javascript"><!-- VI.ifrm.type = 'wel'; VI.ifrm.area = 101; VI.ifrm.lang = 'en'; VI.ifrm.displayWeather(); //--> </script> To show other areas, a different digit must be entered after 'Vi.ifrm.area'. The area codes are as follows: 101 = whole country 111 /about-imo/the-web/iframes/wind-temp-precip/

• 48. Station forecasts, text forecasts or observations

  be copied to your html file where the frame should appear: <script type="text/javascript" src="http://vedur.is/js/iframe.js"></script> <script type="text/javascript"><!-- VI.ifrm.type = 'wst'; VI.ifrm.area = 101; VI.ifrm.lang = 'en'; VI.ifrm.displayWeather(); //--> </script> To show other areas, a different digit must be entered after 'Vi.ifrm.area /about-imo/the-web/iframes/wst-txt-obs/

• 49. norsem_giulia

  Infrasonic and Seismic Signatures of the 2014 Askja Landslide Giulia Barfucci¹, Maurizio Ripepe¹, Giorgio Lacanna¹, Emanuele Marchetti¹, Kristín Jónsdóttir², Kristín S. Vogfjörð² (1) Department of Earth Sciences, University of Firenze, via LaPira, 4, 50121 Firenze, Italy (2) Icelandic Meteorological Office, Reykjavik, IS-108, Iceland Landslides commonly occur at active volcanoes and represent /media/norsem/norsem_giulia.pdf

• 50. Refsgaard_etal-2007-Uncertainty-EMS

  but would have the form of a perfect characterisation of natural variability. 3.4. The uncertainty matrix The uncertainty matrix in Table 1 can be used as a too get an overview of the various sources of uncertainty a modelling study. The matrix is modified after Walke et al. (2003) in such a way that it matches Fig. 3 and that the taxonomy now gives ‘uncertainty type’ in descr tions that indicate /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf