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80 results were found for WA 0821 1305 0400 Biaya Bikin Rumah Minimalis Type 300 Bojonggede Kab Bogor.


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  • 51. BIHN_windrose_2005-2014

    Wind rose BIHN 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 6 Frequency of wind direction (%) Aerodrome Total observations: 28301 Calm: 5.3% Variable winds: 1.6% 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/BIHN_windrose_2005-2014.pdf
  • 52. BITN_windrose_2005-2014

    Wind rose BITN 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 Frequency of wind direction (%) Aerodrome Total observations: 9711 Calm: 5.2% Variable winds: 5.7% 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 /media/vedur/BITN_windrose_2005-2014.pdf
  • 53. BIVO_windrose_2005-2014

    Wind rose BIVO 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 12 14 Frequency of wind direction (%) Aerodrome Total observations: 14082 Calm: 18% Variable winds: 2.1% 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 /media/vedur/BIVO_windrose_2005-2014.pdf
  • 54. The weather app

    the day and can be checked anytime. A personal weather watch will send notifications when certain criteria are met, e.g. a forecast of temperature below zero at your chosen weather station. An interactive weather map shows weather observations at any station in the country. Get the weather app at Google Play Store or Apple App Store. Type VEDUR to find the app and install. Select language under /about-imo/news/nr/2812
  • 55. Glacial outburst floods

    away from the eruption site, but it can also accumulate around the site. Increased accumulation leads to the reservoir becoming unstable and the release of a jökulhlaup. Jökulhlaups from Eyjafjallajökull in 2010 are an example of this type of flood. In large eruptions, such as Katla eruptions underneath Mýrdalsjökull, ice melting can be very rapid and substantial in volume, resulting in large /volcanoes/volcanic-hazards/glacial-outburst/
  • 56. IMO's glaciologist in 'NBC Today'

    geology and geothermal energy it was stated that Iceland's glaciers are melting at an alarming rate. "There's tremendous change all around us," says Matthew J. Roberts, glaciologist at the Icelandic Meteorological Office, in an interview taken on Solheimajokull. "This is a type-site for glacial retreat in Iceland and, in fact, globally." Sólheimajökull is one of several valley glaciers extending /about-imo/news/nr/1412
  • 57. Press release on the l'Aquila sentence

    and minimize the victims of earthquakes. The trial in L'Aquila condemns some of IASPEI's most brilliant scientists, who have dedicated their lives to the reduction of seismic risk. IASPEI is confident that the L'Aquila case will provide the opportunity to develop a proper link between science, policy makers and society in order to avoid any type of miscommunication of information and scientific knowledge /earthquakes-and-volcanism/articles/nr/2568
  • 58. Reading material for the PhD Workshop

    A PhD Workshop on 26-28 August 2012 in Helsinki, directly linked to the 2nd Nordic International Climate Change Adaptation Conference, 29-31 August 2012, Helsinki (see pdf, 0.5 Mb). Material 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343 Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication /nonam/adaption/material/
  • 59. norsem_bryndis

    than 30,000 earthquakes at 5–7 km depth, advancing in short bursts at 0.3–4.7 km/h. Following each surge forward, the seismicity behind the dyke tip dropped, implying that the subsequent dyke opening was mostly aseismic. More detailed analyses of the seismic data recorded by a dense network around the Vatnajökull icecap have revealed small magnitude, long-period (LP or B-type) events which /media/norsem/norsem_bryndis.pdf
  • 60. norsem_giulia

    of this type may represent a serious risk if they occur in tourist spots such as the Askja region. We present observations of the July 21st, 2014 event as recorded by the national infrasonic arrays network installed in the country within the FUTUREVOLC European project. Infrasound released by the event was recorded at a distance of 210 km from Askja volcano. We performed 2D FDTD modeling /media/norsem/norsem_giulia.pdf

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